D.C. Transport Measurements and the Direction of Propagation of Composite Fermion Edge Stat

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PC36c直流电阻测试仪 英文说明书

PC36c直流电阻测试仪 英文说明书

PC36 Series D.C. Resistance Meters Operation InstructionsShanghai Taiou Electronic CO.,Ltd.1.Basic ParametersThe basic parameters are shown as table 1Table 12Technique Requirements2.1environmental conditions2.1.1 environmental temperature 15—25℃2.1.2 relative humidity ≤85%RH2.1.3 power 220V±10%, 48-62Hz2.1.4 Outside of the earth magnetic field, there is no electric field or magnetic field of electric pulse and electric spark in the measurement environment.12.2basic toleranceThe basic tolerance of the measurement is shown as table 2R X:reading of the measurement R m:maximum value of the range2.3Accurate class and maximum toleranceshown as table 3.The accurate class and maximum tolerance isThe rated output currents of the measurement are shown as table 4.22.5Two way current measurementOnce the thermoelectric voltage of the circuit is removed the difference of the result between the positive current measurement and negative current measurement is less than the half of the basic tolerance.2.6 Temperature conversion of the copper wire and aluminum wire2.6.1 temperature conversion rangeenvironmental temperature input ringing from15℃to26℃with the step of 0.1℃.2.6.2 properties of temperature conversionK t = 1/ [1+0.004( t-20 )] = 250 / (230 + t )t: environmental temperature ℃.2.6.3 readout of the meter: R X= R20 = K t*R tR20:resistance at 20℃; R t:resistance at t℃2.7Insulation resistanceInsulation resistance is more than 20 MΩbetween power input leads and outside sell of the meter.2.8Insulation strengthInsulation strength is 50Hz at 1500V (1 minute) between power input leads and outside sell of the meter.3Operation methods3.1 Introduction of panel functionOf which:(1)liquid crystal display (8) measurement state choice switch(2)range choice switch (9) current output terminal “C1”(3)function choice switch (10) voltage input terminal “P1,P2”(4)power switch (11) current output terminal “C2”(5)zero check and balance knob (12) environmental temperature input switch(6)reading hold switch (15-26℃,step 1℃)(7) current direction choice switch (13) environmental temperature input switch(0.0-1.1℃,step 0.1℃)(14)temperature conversion switchNote: The meter has 12 ranges, but the range choice switch (2) has only 6 positions for turning. When the measurement state choice switch (8) is turned to the “normal current” (normal current measurement) position, the screen displays“ THI”, the 6 ranges witch on the upper position of the panel (printed in blue) is effective; and when the switch (8) is turned to the “low current” (low current measurement) position, the screen displays“ TLO”, the 6 ranges witch on the lower position of the panel (printed in black) is effective. The screen displays the maximum value of range ( 2、20 、200 or 2000 ) and the unit of the resistance (Ω、mΩ、μΩ)when measuring3.2 the measuring steps of resistance3.2.1 meter preheat and zero checkTurn the function switch (3) to “zero check”, measurement state choice switch (8) to “ low current”, range choice switch (2) to “200μΩ” to make the meter in the highest sensitivity condition. Turn the power switch (4) to preheat the meter, after 3 minutes, turn zero check knob (5) to make meter value at “00.00”.3.2.2 Connect the meter and the resistor witch is to be measured in the sequence of “C1, P1, P2, C2”with the current junctions outside and the voltage junctions inside, red wires are “C1,P1” and black wires are “ C2, P2 ”. Reduce the possibility of touching the “P1, P2” junctions because the human body will heat the voltage junction, and the effect of thermocouple will influence the result of low resistance measurement.3.2.3 Select suitable range and measurement condition according to the resistor to be measured. The “normal current” measurement state is more accurate in measurement and stronger in the ability against interference. The “low current” measurement state is higher sensitivity and better resolution. If the user can’t estimate the value of the resistor to be measured, please select the higher range and lower current to prevent the resistor from damaging by the high current shock.3.2.4 voltage balance of the measuring circuitTurn function switch (3) from “zero check” to “balance”, The screen will probably display a value which indicates that there exists a no balanced voltage in the measuring circuit. Pay attention, the no balanced voltage is caused by the effect of thermocouple. It is not stable and will reduce in a few minutes, please wait till the value of no balanced voltage is less than 5. Then turn knob (5) again to make meter value between “ –0000 ” to “0000”.3.2.5 resistance measurementTurn function switch (3) to “1.00I ”, the screen displays the resistance value of the resistor to be measured. If it shows “1—”, it means the measurement is under range, please turn range choice switch (2) at clockwise to make measurement value appear. If the value less than 1800, it means the measurement is over range, so turn switch (2) at counter-clockwise to make value in high resolution. If the range issuitable for measurement, readout of the meter is between 1800 to 19999.3.3 reading holdTurn the reading hold switch (6) to “ hold ”, the meter will get into reading hold state, the screen displays “H”, user can record the measurement value conveniently. Normally, the switch (6) is turned to “ run ”, so that the measurement is continuous.3.4 Two-way current measurementIf the resistance of the measurement is less than 0.1Ω, the operation of two-way current measurement should be taken to offset the thermoelectric voltage caused by the effect of thermocouple in the measuring circuit. First, turn the current direction choice switch (7) to “I+”(positive current measurement), t ake down the value of measurement as R I+, and then turn switch (7) to “I-” (negative current measurement), the negative sign appears in front of the resistance value, it indicates the meter has got into the negative current measurement state, take down this value as R I-(omit the negative sign), the result R = (R I++ R I-) / 2 , is more accurate than one-way current measurement.3.5multiple current measurementBecause the temperature resistance coefficient of the copper wire and aluminum wire is rather big, if the measurement current is too big, the wire will be heated so that serious error will be caused. It can be checked by the method of multiple current measurement, to prevent the measurement from too big current.Turn the “function” switch (3) to “ 1.41I ” position (1.41 times of the rated current), to compare with the result under the “ 1.00I ” (rated current). If the difference is within the value required by the national standard, it means the measurement result is valid. Otherwise it means the outcome is not valid because the measurement current is too big. In order to reduce the measurement current please turn switch (3) to “0.707I” position (0.707 times of the rated current). Again, compare it with the result under the “ 1.00I ” (rated current). If the difference is within the value required by the national standard, it means the measurement result under “0.707I” is valid. Otherwise the measurement current is still too big, please select the higher range or turn switch (8) to “ low current ” posit ion, to further reduce the current.3.5 Temperature conversion of the copper wire and aluminum wireWhen measuring the conductor resistance of the copper wire and aluminum wire, set the switch (12) and switch (13) to environmental temperature, and then the readout of the meter will automatically convert to the resistance under the standard temperature—20℃.In this way ,the users don’t need to conversion by the formula themselves. Pay attention to make the measurement of the environmental temperature accurately ( the error less then 0.1℃) .The wires which to be measured must stay in the environment for enough time, so that wire’s temperature totally equals the environmental temperature.Pay more attention, the operation of the automatic temperature conversion is only suitable for the measurements of the resistors which are made of pure copper or pure aluminum (electrolytic copper or electrolytic aluminum). Except this two, neither the standard resistor、the touching resistance and the other substantial resistors;nor the resistors which are made of copper alloy、aluminum alloy、iron alloy and other alloys can be measured with the function of the automatic temperature conversion. The temperature conversion switch (14) should be turned to “OFF ” position, when measuring these resistors. In this state, the function of the temperature conversion is not effective and the readout of the meter is the real resistance of the resistor under the environmental temperature. Because the temperature resistance coefficients of these resistors are rather different from the temperature resistance coefficient of pure copper, it will cause serious errors when the function of temperature conversion is wrongly used.4. Points of attention4.1 The meter is the specialized equipment of measuring the conductor resistance of wires and cables. In order to use the meter correctly and safely, the user must read the operation instructions carefully and completely before using it, because there are many new techniques and special functions in the meter, and it is rather different from other low resistance meters.4.2 When the terminal of “P1, P2, C1, C2” are not connected to the resistor to be measured, the function switch (3) must be turned to “zero check” position. After measurement, the user must turn switch (3) to “zero check” first, and then cut off theconnector. Especially avoid cutting off the measuring circuit when the measurement current is big. When the meter is out of use, please turn switch (3) to “zero check” position too.4.3 Don’t cover the vent of the meter when the meter is being used in order to make heat dissipated well.4.4 The meter should be put in a dry, ventilated place when out of use, avoid severe cold and extremely hot.5 The quality standard and the guarantee of repair5.1 The meter is made on the basis of the standard No. Q/AEXJ3 Shanghai China. 5.2 The manufacturer guarantees to keep the meter in good repair all it’s life, and the repair is free in 12 months expect the trouble of the meter is caused by the wrong use of the user.6 Complete set of the meterProvide following technique files and attachments with every meter:a) product qualified certificate oneb) operation introductions onec) power line oned) measuring cable one pairThe patent has been entitled to this meter. No imitator is allowed.Shanghai Taiou Electronic Co.,LtdAddress: 1, lane74, GuangLing No.1 Road, Shanghai ChinaPost code: 200083Tel: 008621-65607047 65604787 65420430Fax:008621-65607047http:。

TPO51托福阅读passage3:The Role of the Ocean in Controlling Climate原文文本+真题答案

TPO51托福阅读passage3:The Role of the Ocean in Controlling Climate原文文本+真题答案

TPO51托福阅读passage3:The Role of the Oceanin Controlling Climate原文文本+真题答案第三篇:社会学The Role of the Ocean in Controlling ClimateTo predict what the climate will be like in the future, scientists must rely on sophisticated computer models. These models use mathematical equations to represent physical processes and interactions in the atmosphere, ocean, and on land. A starting point is usually based on current measurements or estimates of past conditions. Then, using a spherical grid laid out over the entire globe,thousands of calculations are performed at grid intersections to represent and assess how conditions in the air, in the sea, and on land will change over time. Because of their complexity and size, supercomputers are used to run full-scale climate models. Much of the uncertainty in their outputs comes from the way that various aspects of the climate are represented by different models, and even more so, because there are aspects of climate that are not well understood—one of which is how the ocean impacts climate.The ocean’s role in global warming stems principally from its huge capacity to absorb carbon dioxide and to store and transport heat. In the sea, photosynthesis by marine plants and algae, especially phytoplankton, removes great quantities of carbon dioxide from the atmosphere. Hence, the greater the growth (productivity) of phytoplankton in the sea, the greater the removal of carbon dioxide. But what controls the ocean’s productivity? There are several limiting factors, but results from a recent experiment suggest that in areas of the ocean where other nutrients are plentiful, iron may be one ofthe most important and, until recently, unrecognized variables controlling phytoplankton production. Some have proposed a radical, highly controversial and uncertain means to counteract global warming —adding iron to the oceans to induce phytoplankton blooms. Perhaps increased phytoplankton growth would use up a significant amount of carbon dioxide in the atmosphere, but perhaps not, and there might well be side effects that could be detrimental to the ocean ecosystem.Within the ocean, the production of limestone, in the form of calcium carbonate skeletons or shells, also reduces atmospheric carbon dioxide. However, when deposits of limestone become exposed and weathered on land or are recycled in the sea, carbon dioxide is released back into the atmosphere. What is not well understood is how much carbon dioxide resides in the sea and at what rate it is taken up and recycled. Relatively new research has also discovered beneath the sea a new and potentially significant threat to skyrocketing Earth temperature: gas hydrates. Gas hydrates are a solid, crystalline form of water, like ice, except that they contain additional gas, typically methane, and are often found stored in ocean sediments. Increased ocean temperatures could cause gas hydrates to dissociate, releasing massive amounts of methane gas into the atmosphere and cause undersea landslides in the process. Consequently, hydrates may, if released, significantly increase global warming as well as create a geologic hazard to offshore drilling operations.The ocean is also a great reservoir and transporter of heat. Heat from the ocean warms the atmosphere and fuels tropical storms. Heat is transported by currents from the equator to the poles. Ocean circulation is strongly controlled by wind and by the sea’s balance of salt and heat. Scientists think that climate warming may slow down circulation, while cooling may speed it up, but these responses are not well understood. Evaporation from the ocean also supplies the precipitation that creates fields of snow and ice at high latitudes. Snow and ice coverage change thereflectivity Earth’s surface and are an important influence on how much incoming radiation is either absorbed or reflected. Furthermore, clouds and water vapor in the atmosphere come mainly from the sea and strongly influence climate. Surprisingly, clouds are one of the least understood and most poorly modeled parts of the climate change equation. Most climate modeling grids fail to take into account common-sized cloud formations. Aerosols, tiny particles of soot, dust, and other materials, are thought to seed cloud formation scatter incoming radiation and promote cooling, but this effect, which would counteract warming, is also only superficially understood. Computer models of climate change must take into account all of the processes within the ocean, over land, and in the sky that potentially influence warming. No wonder there is such uncertainty.题目Paragraph 1To predict what the climate will be like in the future, scientists must rely on sophisticated computer models. These models use mathematical equations to represent physical processes and interactions in the atmosphere, ocean, and on land. A starting point is usually based on current measurements or estimates of past conditions. Then, using a spherical grid laid out over the entire globe, thousands of calculations are performed at grid intersections to represent and assess how conditions in the air, in the sea, and on land will change over time.Because of their complexity and size, supercomputers are used to run full-scale climate models. Much of the uncertainty in their outputs comes from the way that various aspects of the climate are represented by different models, and even more so, because there are aspects of climate that are not well understood—one of which is how the ocean impacts climate.1.According to paragraph 1, the results of full-scale climate models are questionable in part becauseA.the supercomputers used for such modeling are large and complexB.thousands of calculations have to be performed to assess conditionsC.past conditions cannot always be estimated accuratelyD.there are multiple ways to represent the same aspect of climate Paragraph 2The ocean’s role in global warming stems principally from its huge capacity to absorb carbon dioxide and to store and transport heat. In the sea, photosynthesis by marine plants and algae, especially phytoplankton, removes great quantities of carbon dioxide from the atmosphere. Hence, the greater the growth (productivity) of phytoplankton in the sea, the greater the removal of carbon dioxide. But whatcontrols the ocean’s productivity? There are several limiting factors, but results from a recent experiment suggest that in areas of the ocean where other nutrients are plentiful, iron may be one of the most important and, until recently, unrecognized variables controlling phytoplankton production. Some have proposed a radical, highly controversial and uncertain means to counteract global warming—adding iron to the oceans to induce phytoplankton blooms. Perhaps increased phytoplankton growth would use up a significant amount of carbon dioxide in the atmosphere, but perhaps not, and there might well be side effects that could be detrimental to the ocean ecosystem.2.The word “principally”in the passage is closet in meaning toA.obviouslyB.apparentlyC.mainlyD.originally3.Which of the sentences below best expresses the essential information in the highlighted sentence in the passage? Incorrect choices change the meaning in important ways or leave out essential information.A.Iron may be one of the most important factors in controlling phytoplankton production in ocean waters that are rich in other nutrients.B.Results from a recent experiment suggest that several factors limiting phytoplankton production in ocean waters have gone unrecognized.C.Although it was not recognized until recently, nutrients are plentiful in areas of the ocean where iron controls phytoplankton production.D.Until recently, the importance of iron was not taken into account in experiments concerning phytoplankton production.4.The word “controversial”in the passage is closest in meaning toA.experimentalB.fascinatingC.producing disagreementD.demonstrating poor judgment5.The word “induce”in the passage is closest in meaning toA.supply nutrients toB.cause the formation ofC.expandD.strengthen6.According to paragraph 2, how might increasing phytoplankton growth help lower global temperatures?A.By cooling the oceansB.By decreasing carbon dioxide levels in the oceanC.By reducing the amount of carbon dioxide in the atmosphereD.By transporting heat from the ocean’s surface to deeper levelsParagraph 3Within the ocean, the production of limestone, in the form of calcium carbonate skeletons or shells, also reduces atmospheric carbon dioxide. However, when deposits of limestone become exposed and weathered on land or are recycled in the sea, carbon dioxide is released back into the atmosphere. What is not wellunderstood is how much carbon dioxide resides in the sea and at what rate it is taken up and recycled. Relatively new research has also discovered beneath the sea a new and potentially significant threat to skyrocketing Earth temperature: gas hydrates. Gas hydrates are a solid, crystalline form of water, like ice, except that they contain additional gas, typically methane, and are often found stored in ocean sediments. Increased ocean temperatures could cause gas hydrates to dissociate, releasing massive amounts of methane gas into the atmosphere and cause undersea landslides in the process. Consequently, hydrates may, if released, significantly increase global warming as well as create a geologic hazard to offshore drilling operations.7.According to paragraph 3, which of the following reduces atmospheric carbon dioxide?A.The weathering of limestoneB.The production of limestoneC.The recycling of carbon dioxideD.The presence of methane in gas hydrates8.According to paragraph 3, why are gas hydrates a possible threat to the global climate?A.If disturbed by offshore drilling, they can destroy limestone deposits.B.They can replace regular ice at certain locations.C.If melted, they may release a lot of carbon dioxide into the atmosphere.D.They contain a lot of methane, which may be released as the ocean warms Paragraph 4The ocean is also a great reservoir and transporter of heat. Heat from the ocean warms the atmosphere and fuels tropical storms. Heat is transported by currents from the equator to the poles. Ocean circulation is strongly controlled by wind and by the sea’s balance of salt and heat. Scientists think that climate warming may slow down circulation, while cooling may speed it up, but these responses are not well understood. Evaporation from the ocean also supplies the precipitation that creates fields of snow and ice at high latitudes. Snow and ice coverage change the reflectivity Earth’s surface and are an important influence on how much incoming radiation is either absorbed or reflected. Furthermore, clouds and water vapor in the atmosphere come mainly from the sea and strongly influence climate. Surprisingly, clouds are one of the least understood and most poorly modeled parts of the climate change equation. Most climate modeling grids fail to take into account common-sized cloud formations. Aerosols, tiny particles of soot, dust, and other materials, are thought to seed cloud formation scatter incoming radiation and promote cooling, but this effect, which would counteract warming, is also only superficially understood. Computer models of climate change must take into account all of the processes within the ocean, over land, and in the sky that potentially influence warming. No wonder there is such uncertainty.9.The word “fuels”in the passage is closest in meaning toA.provides energy forB.determines the route ofC.carriesD.breaks up10.Which of the following is NOT mentioned in paragraph 4 as a way in which the ocean affects the climate?A.It stores heatB.It moves heat from the equator toward the poles.C.It speeds up wind circulation.D.It warms up the atmosphere.11.Paragraph 4 suggests that a significant decrease in snow and ice fields at high latitudes would have what effect?A.More clouds and water vapor would be produced in the atmosphere.B.More of the Sun’s radiation would be absorbed by Earth.C.The oceans would cool more quickly.D.More precipitation would occur at low latitudes.12.Why does the author mention that “Most climate modeling grids fail to take into account common-sized cloud formations”?A.To suggest why the influence of clouds on climate change is still undeterminedB.To explain why research on climate change does not focus on cloudsC.To help explain why it is unclear whether aerosols have the effect of counteracting warmingD.To explain in part why scientists are uncertain how much incoming radiation is absorbed or reflectedParagraph 3Within the ocean, the production of limestone, in the form of calcium carbonate skeletons or shells, also reduces atmospheric carbon dioxide. ■However, when deposits of limestone become exposed and weathered on land or are recycled in the sea, carbon dioxide is released back into the atmosphere. ■What is not well understood is how much carbon dioxide resides in the sea and at what rate it is taken up and recycled. ■Relatively new research has also discovered beneath the sea a new and potentially significant threat to skyrocketing Earth temperature: gas hydrates. ■Gas hydrates are a solid, crystalline form of water, like ice, except that they contain additional gas, typically methane, and are often found stored in ocean sediments. Increased oceantemperatures could cause gas hydrates to dissociate, releasing massive amounts of methane gas into the atmosphere and cause undersea landslides in the process. Consequently, hydrates may, if released, significantly increase global warming as well as create a geologic hazard to offshore drilling operations.13.Look at the four squares [■] that indicate where the following sentence could be added to the passageNor is carbon dioxide the only gaseous substance in the ocean that may affect climate.Where would the sentence best fit?14.Directions: An introductory sentence for a brief summary of the passage is provided below. Complete the summary by selected THREE answer choices that express the most important ideas in the passage. Some sentences do not belong in the summary because they express ideas that are not presented in the passage or are minor ideas in the passage. This question is worth 2 points.The oceans affect the climate in numerous ways, some of which are poorly understood and therefore cannot be accurately modeled in computer climate programs.Answer ChoicesA.Estimates of future conditions are entered into supercomputers to calculate climate possibilities at various places on earth.B.Oceans absorb a great deal of carbon dioxide from the air through limestone production and photosynthesis or phytoplankton.C.Gases are stored in the sea in the form of shells and hydrates, but gases stored in these ways can be recycled to the atmosphere where they may cause warming.D.The ocean's capacity to absorb carbon dioxide remains great despite recent reduction of marine plant nutrients such as iron.E.Ocean circulation is strongly controlled by wind and by the sea s balance or salt and heat.F.The ocean bolds and moves a great deal of heat, and as waterevaporates, it produces clouds, snow, and ice, which all affect global temperatures.参考答案1-5:DCACB6-10:CBDAC11-13:BAC14:BCF文章来源:雷哥托福。

精品文档TPO51托福阅读passage3:The Role of the Ocean in Controlling Climate原文文本 真题答案

精品文档TPO51托福阅读passage3:The Role of the Ocean in Controlling Climate原文文本 真题答案

TPO51托福阅读passage3:The Role of the Oceanin Controlling Climate原文文本+真题答案第三篇:社会学The Role of the Ocean in Controlling ClimateTo predict what the climate will be like in the future, scientists must rely on sophisticated computer models. These models use mathematical equations to represent physical processes and interactions in the atmosphere, ocean, and on land. A starting point is usually based on current measurements or estimates of past conditions. Then, using a spherical grid laid out over the entire globe,thousands of calculations are performed at grid intersections to represent and assess how conditions in the air, in the sea, and on land will change over time. Because of their complexity and size, supercomputers are used to run full-scale climate models. Much of the uncertainty in their outputs comes from the way that various aspects of the climate are represented by different models, and even more so, because there are aspects of climate that are not well understood—one of which is how the ocean impacts climate.The ocean’s role in global warming stems principally from its huge capacity to absorb carbon dioxide and to store and transport heat. In the sea, photosynthesis by marine plants and algae, especially phytoplankton, removes great quantities of carbon dioxide from the atmosphere. Hence, the greater the growth (productivity) of phytoplankton in the sea, the greater the removal of carbon dioxide. But what controls the ocean’s productivity? There are several limiting factors, but results from a recent experiment suggest that inareas of the ocean where other nutrients are plentiful, iron may be one of the most important and, until recently, unrecognized variables controlling phytoplankton production. Some have proposed a radical, highly controversial and uncertain means to counteract global warming —adding iron to the oceans to induce phytoplankton blooms. Perhaps increased phytoplankton growth would use up a significant amount of carbon dioxide in the atmosphere, but perhaps not, and there might well be side effects that could be detrimental to the ocean ecosystem.Within the ocean, the production of limestone, in the form of calcium carbonate skeletons or shells, also reduces atmospheric carbon dioxide. However, when deposits of limestone become exposed and weathered on land or are recycled in the sea, carbon dioxide is released back into the atmosphere. What is not well understood is how much carbon dioxide resides in the sea and at what rate it is taken up and recycled. Relatively new research has also discovered beneath the sea a new and potentially significant threat to skyrocketing Earth temperature: gas hydrates. Gas hydrates are a solid, crystalline form of water, like ice, except that they contain additional gas, typically methane, and are often found stored in ocean sediments. Increased ocean temperatures could cause gas hydrates to dissociate, releasing massive amounts of methane gas into the atmosphere and cause undersea landslides in the process. Consequently, hydrates may, if released, significantly increase global warming as well as create a geologic hazard to offshore drilling operations.The ocean is also a great reservoir and transporter of heat. Heat from the ocean warms the atmosphere and fuels tropical storms. Heat is transported by currents from the equator to the poles. Ocean circulation is strongly controlled by wind and by the sea’s balance of salt and heat. Scientists think that climate warming may slow down circulation, while cooling may speed it up, but these responses are not well understood. Evaporation from the ocean also supplies theprecipitation that creates fields of snow and ice at high latitudes. Snow and ice coverage change thereflectivity Earth’s surface and are an important influence on how much incoming radiation is either absorbed or reflected. Furthermore, clouds and water vapor in the atmosphere come mainly from the sea and strongly influence climate. Surprisingly, clouds are one of the least understood and most poorly modeled parts of the climate change equation. Most climate modeling grids fail to take into account common-sized cloud formations. Aerosols, tiny particles of soot, dust, and other materials, are thought to seed cloud formation scatter incoming radiation and promote cooling, but this effect, which would counteract warming, is also only superficially understood. Computer models of climate change must take into account all of the processes within the ocean, over land, and in the sky that potentially influence warming. No wonder there is such uncertainty.题目Paragraph 1To predict what the climate will be like in the future, scientists must rely on sophisticated computer models. These models use mathematical equations to represent physical processes and interactions in the atmosphere, ocean, and on land. A starting point is usually based on current measurements or estimates of past conditions. Then, using a spherical grid laid out over the entire globe, thousands of calculations are performed at grid intersections to represent and assess how conditions in the air, in the sea, and on land will change over time.Because of their complexity and size, supercomputers are used to run full-scale climate models. Much of the uncertainty in their outputs comes from the way that various aspects of the climate are represented by different models, and even more so, because there are aspects ofclimate that are not well understood—one of which is how the ocean impacts climate.1.According to paragraph 1, the results of full-scale climate models are questionable in part becauseA.the supercomputers used for such modeling are large and complexB.thousands of calculations have to be performed to assess conditionsC.past conditions cannot always be estimated accuratelyD.there are multiple ways to represent the same aspect of climate Paragraph 2The ocean’s role in global warming stems principally from its huge capacity to absorb carbon dioxide and to store and transport heat. In the sea, photosynthesis by marine plants and algae, especially phytoplankton, removes great quantities of carbon dioxide from the atmosphere. Hence, the greater the growth (productivity) of phytoplankton in the sea, the greater the removal of carbon dioxide. But whatcontrols the ocean’s productivity? There are several limiting factors, but results from a recent experiment suggest that in areas of the ocean where other nutrients are plentiful, iron may be one of the most important and, until recently, unrecognized variables controlling phytoplankton production. Some have proposed a radical, highly controversial and uncertain means to counteract global warming—adding iron to the oceans to induce phytoplankton blooms. Perhaps increased phytoplankton growth would use up a significant amount of carbon dioxide in the atmosphere, but perhaps not, and there might well be side effects that could be detrimental to the ocean ecosystem.2.The word “principally”in the passage is closet in meaning toA.obviouslyB.apparentlyC.mainlyD.originally3.Which of the sentences below best expresses the essential information in the highlighted sentence in the passage? Incorrect choices change the meaning in important ways or leave out essential information.A.Iron may be one of the most important factors in controlling phytoplankton production in ocean waters that are rich in other nutrients.B.Results from a recent experiment suggest that several factors limiting phytoplankton production in ocean waters have gone unrecognized.C.Although it was not recognized until recently, nutrients are plentiful in areas of the ocean where iron controls phytoplankton production.D.Until recently, the importance of iron was not taken into account in experiments concerning phytoplankton production.4.The word “controversial”in the passage is closest in meaning toA.experimentalB.fascinatingC.producing disagreementD.demonstrating poor judgment5.The word “induce”in the passage is closest in meaning toA.supply nutrients toB.cause the formation ofC.expandD.strengthen6.According to paragraph 2, how might increasing phytoplanktongrowth help lower global temperatures?A.By cooling the oceansB.By decreasing carbon dioxide levels in the oceanC.By reducing the amount of carbon dioxide in the atmosphereD.By transporting heat from the ocean’s surface to deeper levels Paragraph 3Within the ocean, the production of limestone, in the form of calcium carbonate skeletons or shells, also reduces atmospheric carbon dioxide. However, when deposits of limestone become exposed and weathered on land or are recycled in the sea, carbon dioxide is released back into the atmosphere. What is not wellunderstood is how much carbon dioxide resides in the sea and at what rate it is taken up and recycled. Relatively new research has also discovered beneath the sea a new and potentially significant threat to skyrocketing Earth temperature: gas hydrates. Gas hydrates are a solid, crystalline form of water, like ice, except that they contain additional gas, typically methane, and are often found stored in ocean sediments. Increased ocean temperatures could cause gas hydrates to dissociate, releasing massive amounts of methane gas into the atmosphere and cause undersea landslides in the process. Consequently, hydrates may, if released, significantly increase global warming as well as create a geologic hazard to offshore drilling operations.7.According to paragraph 3, which of the following reduces atmospheric carbon dioxide?A.The weathering of limestoneB.The production of limestoneC.The recycling of carbon dioxideD.The presence of methane in gas hydrates8.According to paragraph 3, why are gas hydrates a possible threat to the global climate?A.If disturbed by offshore drilling, they can destroy limestone deposits.B.They can replace regular ice at certain locations.C.If melted, they may release a lot of carbon dioxide into the atmosphere.D.They contain a lot of methane, which may be released as the ocean warms Paragraph 4The ocean is also a great reservoir and transporter of heat. Heat from the ocean warms the atmosphere and fuels tropical storms. Heat is transported by currents from the equator to the poles. Ocean circulation is strongly controlled by wind and by the sea’s balance of salt and heat. Scientists think that climate warming may slow down circulation, while cooling may speed it up, but these responses are not well understood. Evaporation from the ocean also supplies the precipitation that creates fields of snow and ice at high latitudes. Snow and ice coverage change the reflectivity Earth’s surface and are an important influence on how much incoming radiation is either absorbed or reflected. Furthermore, clouds and water vapor in the atmosphere come mainly from the sea and strongly influence climate. Surprisingly, clouds are one of the least understood and most poorly modeled parts of the climate change equation. Most climate modeling grids fail to take into account common-sized cloud formations. Aerosols, tiny particles of soot, dust, and other materials, are thought to seed cloud formation scatter incoming radiation and promote cooling, but this effect, which would counteract warming, is also only superficially understood. Computer models of climate change must take into account all of the processes within the ocean, over land, and in the sky that potentially influence warming. No wonder there is such uncertainty.9.The word “fuels”in the passage is closest in meaning toA.provides energy forB.determines the route ofC.carriesD.breaks up10.Which of the following is NOT mentioned in paragraph 4 as a way in which the ocean affects the climate?A.It stores heatB.It moves heat from the equator toward the poles.C.It speeds up wind circulation.D.It warms up the atmosphere.11.Paragraph 4 suggests that a significant decrease in snow and ice fields at high latitudes would have what effect?A.More clouds and water vapor would be produced in the atmosphere.B.More of the Sun’s radiation would be absorbed by Earth.C.The oceans would cool more quickly.D.More precipitation would occur at low latitudes.12.Why does the author mention that “Most climate modeling grids fail to take into account common-sized cloud formations”?A.To suggest why the influence of clouds on climate change is still undeterminedB.To explain why research on climate change does not focus on cloudsC.To help explain why it is unclear whether aerosols have the effect of counteracting warmingD.To explain in part why scientists are uncertain how much incoming radiation is absorbed or reflectedParagraph 3Within the ocean, the production of limestone, in the form of calcium carbonate skeletons or shells, also reduces atmospheric carbon dioxide. ■However, when deposits of limestone become exposed andweathered on land or are recycled in the sea, carbon dioxide is released back into the atmosphere. ■What is not well understood is how much carbon dioxide resides in the sea and at what rate it is taken up and recycled. ■Relatively new research has also discovered beneath the sea a new and potentially significant threat to skyrocketing Earth temperature: gas hydrates. ■Gas hydrates are a solid, crystalline form of water, like ice, except that they contain additional gas, typically methane, and are often found stored in ocean sediments. Increased ocean temperatures could cause gas hydrates to dissociate, releasing massive amounts of methane gas into the atmosphere and cause undersea landslides in the process. Consequently, hydrates may, if released, significantly increase global warming as well as create a geologic hazard to offshore drilling operations.13.Look at the four squares [■] that indicate where the following sentence could be added to the passageNor is carbon dioxide the only gaseous substance in the ocean that may affect climate.Where would the sentence best fit?14.Directions: An introductory sentence for a brief summary of the passage is provided below. Complete the summary by selected THREE answer choices that express the most important ideas in the passage. Some sentences do not belong in the summary because they express ideas that are not presented in the passage or are minor ideas in the passage. This question is worth 2 points.The oceans affect the climate in numerous ways, some of which are poorly understood and therefore cannot be accurately modeled in computer climate programs.Answer ChoicesA.Estimates of future conditions are entered into supercomputers to calculate climate possibilities at various places on earth.B.Oceans absorb a great deal of carbon dioxide from the air throughlimestone production and photosynthesis or phytoplankton.C.Gases are stored in the sea in the form of shells and hydrates, but gases stored in these ways can be recycled to the atmosphere where they may cause warming.D.The ocean's capacity to absorb carbon dioxide remains great despite recent reduction of marine plant nutrients such as iron.E.Ocean circulation is strongly controlled by wind and by the sea s balance or salt and heat.F.The ocean bolds and moves a great deal of heat, and as water evaporates, it produces clouds, snow, and ice, which all affect global temperatures.参考答案1-5:DCACB6-10:CBDAC11-13:BAC14:BCF文章来源:雷哥托福倚窗远眺,目光目光尽处必有一座山,那影影绰绰的黛绿色的影,是春天的颜色。

杰尼奥公司的Raman光谱仪使用培训课程说明书

杰尼奥公司的Raman光谱仪使用培训课程说明书

6Who should attendFrom Monday 9 am to Wednesday 5:30 pmDates: February 11-13, 2019 May 13-15, 2019 June 24-26, 2019 October 7-9, 2019November 18-20, 2019Users of HORIBA Scientific Raman spectrometers • A cquire theoretical and practical knowledge on Raman spectrometers • L earn how to use the software • L earn methodology for method development and major analytical parameters • H ow to set up an analytical strategy with an unknown sample • H ow to interpret results• L earn how to follow the performances of theRaman spectrometer over the time.Day 1• The theory of the Raman principle • R aman Instrumentation • P ractical session – System and software presentation, Acquisition Parameters: - L abSpec 6 presentation and environment: useraccounts, file handling, display of data, basic functions - S et up of acquisition parameters and singlespectra measurement - Templates & ReportsDay 2• Analysis of Raman spectra • P ractical session: Raman spectrum measurement and Database Search - O ptimization of the parameters: how to chosethe laser, the grating, the confocal hole, the laser power- How to use the polarization options - Library Search using KnowItAll software - How to create databasesRaman imaging • H ow to make a Raman image (1D, 2D and 3D) • D ata evaluation: cursors, CLS fitting, peakfitting•Image rendering, 3D datasets •Fast mapping using SWIFT XSDay 3Data processing• Processing on single spectra and datasets • Baseline correction • Smoothing • Normalization• Spectra subtraction, averaging • Data reduction • Methods• Practical exercisesCustomer samples: Bring your own samples!Duration: 3 daysReference: RAM1Raman Microscopy for Beginners7Acquire technical skills on DuoScan, Ultra Low Frequency (ULF), Particle Finder or TERS.Users of HORIBA Scientific Raman spectrometers who already understand the fundamentals of Raman spectroscopy and know how to use HORIBA Raman system and LabSpec Software. It is advised to participate in the basic Raman training first (RAM1).Introduction to DuoScan• Principle and hardwareDuoScan Macrospot• Practical examplesDuoScan MacroMapping• Practical examplesDuoScan Stepping Mode• Practical examplesCustomer samples: Bring your own samples!Presentation of the ULF kit• Principle and requirements • Application examplesInstallation of the ULF kitIntroduction to Particle Finder• Principle and requirementsPractical session• Demo with known sample• Customer samples: Bring your own samples!Practical session• Demo with known samplesCustomers samples: Bring your own samples! Presentation of the TERS technique• Principle and requirements • Application examplesDemo TERS• Presentation of the different tips and SPM modes • Laser alignment on the tip • T ERS spectra and TERS imaging on known samplesPractical session• Hands-on on demo samples (AFM mode)• Laser alignment on the tip • T ERS spectra and TERS imaging on known samplesRaman Options: DuoScan, Ultra Low Frequency, Particle Finder, TERS8Users of HORIBA Scientific Raman spectrometers who already understand the fundamentals of Raman spectroscopy and know how to use HORIBA Raman system and labSpec Software. It is adviced to participate in the basic Raman training first.Who should attendDates: February 14, 2019 June 27, 2019November 21, 2019Duration: 1 dayReference: RAM2From 9 am to 5:30 pm• Acquire theoretical and practical knowledge on SERS (Surface Enhanced Raman Spectroscopy)• Know how to select your substrate • Interpret resultsRaman SERSIntroduction to SERSPresentation of the SERS technique • Introduction: Why SERS?• What is SERS?• Surface Enhanced Raman basics • SERS substratesIntroduction to the SERS applications• Examples of SERS applications • Practical advice • SERS limitsDemo on known samplesCustomer samples: Bring your own samples!Raman Multivariate Analysis9Users of HORIBA Scientific Raman spectrometerswho already understand the fundamentals of Ramanspectroscopy and know how to use HORIBA Ramansystem and LabSpec Software. It is advised toparticipate in the basic Raman training first (RAM1).• Understand the Multivariate Analysis module• Learn how to use Multivariate Analysis for data treatment• Perform real case examples of data analysis on demo and customer dataIntroduction to Multivariate Analysis• Univariate vs. Multivariate analysis• Introduction to the main algorithms: decomposition (PCA and MCR), classification and quantification (PLS)Practical work on known datasets (mapping)• CLS, PCA, MCRIntroduction to classification• HCA, k-means• Demo with known datasetsIntroduction to Solo+MIA• Presentation of Solo+MIA Array• Demo with known datasetsData evaluation: cursors, CLS fitting, peak fitting• Fast mapping using SWIFT XSObjective: Being able to select the good parameters for Raman imaging and to perform data processScanning Probe Microscopy (SPM)• Instrumentation• T he different modes (AFM, STM, Tuning Fork) and signals (Topography, Phase, KPFM, C-AFM, MFM,PFM)Practical session• Tips and sample installation• Molecular resolution in AFM tapping mode• M easurements in AC mode, contact mode, I-top mode, KPFM• P resentation of the dedicated tips and additional equipment• O bjective: Being able to use the main AFM modes and optimize the parametersimaging)Practical session• Hands-on on demo samples (AFM mode)• Laser alignment on the tip• T ERS spectra and TERS imaging on known sample Day 3TERS Hands-on• T ERS measurements, from AFM-TERS tip installation to TERS mapping.• TERS measurements on end users samples.• Bring your own samples!28Practical informationCourses range from basic to advanced levels and are taught by application experts. The theoretical sessions aim to provide a thorough background in the basic principles and techniques. The practical sessions are directed at giving you hands-on experience and instructions concerning the use of your instrument, data analysis and software. We encourage users to raise any issues specific to their application. At the end of each course a certificate of participation is awarded.Standard, customized and on-site training courses are available in France, G ermany, USA and also at your location.Dates mentionned here are only available for HORIBA France training center.RegistrationFill in the form and:• Emailitto:***********************• Or Fax it to: +33 (0)1 69 09 07 21• More information: Tel: +33 (0)1 69 74 72 00General InformationThe invoice is sent at the end of the training.A certificate of participation is also given at the end of the training.We can help you book hotel accommodations. Following your registration, you will receive a package including training details and course venue map. We will help with invitation letters for visas, but HORIBA FRANCE is not responsible for any visa refusal. PricingRefreshments, lunches during training and handbook are included.Hotel transportation, accommodation and evening meals are not included.LocationDepending on the technique, there are three locations: Longjumeau (France, 20 km from Paris), Palaiseau (France, 26 km from Paris), Villeneuve d’Ascq (France 220 km from Paris) or at your facility for on-site training courses. Training courses can also take place in subsidiaries in Germany or in the USA.Access to HORIBA FRANCE, Longjumeau HORIBA FRANCE SAS16 - 18 rue du canal91165 Longjumeau - FRANCEDepending on your means of transport, some useful information:- if you are arriving by car, we are situated near the highways A6 and A10 and the main road N20- if you are arriving by plane or train, you can take the train RER B or RER C that will take you not far from our offices. (Around 15 €, 150 € by taxi from Charles de Gaulle airport, 50 € from Orly airport).We remain at your disposal for any information to access to your training place. You can also have a look at our web site at the following link:/scientific/contact-us/france/visi-tors-guide/Access to HORIBA FRANCE, Palaiseau HORIBA FRANCE SASPassage Jobin Yvon, Avenue de la Vauve,91120 Palaiseau - FRANCEFrom Roissy Charles de Gaulle Airport By Train • T ake the train called RER B (direction Saint RemyLes Chevreuse) and stop at Massy-Palaiseaustation• A t Massy-Palaiseau station, take the Bus 91-06C or 91-10 and stop at Fresnel• T he company is a 5 minute walk from the station,on your left, turn around the traffic circle and youwill see the HORIBA building29 Practical InformationAround 150 € by taxi from Charles de Gaulle airport. From Orly Airport By Train• A t Orly airport, take the ORLYVAL, which is ametro line that links the Orly airport to the AntonyRER station• A t Antony station, take the RER B (direction StRemy Les Chevreuse) and stops at Massy-Palai-seau station• A t Massy-Palaiseau station, take the Bus 91-06C, 91-06 B or 91-10 stop at Fresnel• T he company is 5 minutes walk from the station,on your left, turn around the traffic circle and youwill see the HORIBA building• O r at Orly take the Bus 91-10 stop at Fresnel.The company is 5 minutes walk from the station,on your left, turn around the traffic circle and youwill see the HORIBA building. We remain at yourdisposal for any information to access to your trainingplace. You can also have a look at our web site at thefollowing link:/scientific/contact-us/france/visi-tors-guide/Around 50 € by taxi from Orly airport.Access to HORIBA FRANCE, Villeneuve d’Ascq HORIBA Jobin Yvon SAS231 rue de Lille,59650 Villeneuve d’Ascq - FRANCEBy Road from ParisWhen entering Lille, after the exit «Aéroport de Lequin», take the direction «Bruxelles, Gand, Roubaix». Immmediatly take the direction «Gand / Roubaix» (N227) and No «Bruxelles» (A27) Nor «Valenciennes» (A23).You will then arrive on the ringroad around Villeneuve d’Ascq. Take the third exit «Pont de Bois».At the traffic light turn right and follow the road around, (the road will bend left then right). About 20m further on you will see the company on the right hand side where you can enter the car park.By Road from Belgium (GAND - GENT)Once in France, follow the motorway towards Lille. After «Tourcoing / Marcq-en-Baroeul», follow on the right hand side for Villeneuve d’Ascq. Take the exit «Flers Chateau» (This is marked exit 6 and later exit 5 - but it is the same exit). (You will now be following a road parallel to the mo-torway) Stay in the middle lane and go past two sets of traffic lights; at the third set of lighte, move into the left hand lane to turn under the motorway.At the traffic lights under the motorway go straight, (the road shall bend left then right). About 20 m further you shall see the company on the right hand side where you can enter the car park.AeroplaneFrom the airport Charles de Gaulle take the direction ‘Ter-minal 2’ which is also marked TGV (high speed train); where you can take the train to ‘Lille Europe’.Train - SNCFThere are two train stations in Lille - Lille Europe or Lille Flandres. Once you have arrived at the station in Lille you can take a taxi for HORIBA Jobin Yvon S.A.S., or you can take the underground. Please note both train stations have stations for the underground.Follow the signs:1. From the station «Lille Flandres», take line 1, direction «4 Cantons» and get off at the station «Pont de bois».2. From the station «Lille Europe», take line 2, direction «St Philibert» and get off at the following station «Gare Lille Flandres» then take line 1, direction «4 Cantons» and get off at the station «Pont de Bois».BusBus n°43, direction «Hôtel de Ville de Villeneuve d’Ascq», arrêt «Baudoin IX».InformationRegistration: Fill inthe form and send it back by FAX or Email four weeks before beginning of the training.Registration fees: the registration fees include the training courses and documentation. Hotel, transportation and living expenses are not included except lunches which are taken in the HORIBA Scientific Restaurant during the training.Your contact: HORIBA FRANCE SAS, 16-18 rue du Canal, 91165 Longjumeau, FRANCE Tel: + 33 1 64 74 72 00Fax: + 33 1 69 09 07 21E-Mail:***********************Siret Number: 837 150 366 00024Certified ISO 14001 in 2009, HORIBA Scientific is engaged in the monitoring of the environmental impact of its activitiesduring the development, manufacture, sales, installation and service of scientific instruments and optical components. Trainingcourses include safety and environmental precautions for the use of the instrumentsHORIBA Scientific continues contributing to the preservation of theglobal environment through analysis and measuring technologymentisnotcontractuallybindingunderanycircumstances-PrintedinFrance-©HORIBAJobinYvon1/219。

build443

build443

CONCRETE, HARDENED:ACCELERATED CHLORIDE PENETRATIONKey words:Test method, hardenednon-steady state diffusionconcrete,chloride penetration,1SCOPEThis Nordtest method specifies a procedure for the deter-mination of penetration parameters for estimating the resist-ance against chloride penetration into hardened concrete orother cement-based materials.The resistance against chloride penetration is determined by accelerated testing.2FIELD OF APPLICATIONThe method is applicable to test specimens from existing structures and to new samples older than 28 maturity-days. The concrete test specimens must be free from construction faults such as cavities and visible cracks.It is important to keep in mind that the values for the chloride penetration parameters are dependent on concrete maturity. Especially concretes containing pozzolans will not havereached optimum maturity after a period of 28 maturity-days, which is the specified minimum curing time before exposure. Deviations from the requirements of the method concerning exposure temperature, exposure time, together with the com-position and the chloride concentration of the exposure liquid,can be made where required by the purpose of the test. In caseof any deviations, it must be stated in the test report that the results are obtained from a modified test and the deviations must be specified.Parameters of importance for the resistance against chloride penetration are e.g. composition, workmanship, surfacing,curing, age.3REFERENCESNT BUILD 202, 2nd ed. Approved 1984-05. Concrete, hard-ened: Sampling and treatment of cores for strength tests.NT BUILD 208, 2nd ed. Approved 1984-05.Concrete, hard-ened: Chloride content.UDC 622.434DEFINITIONSChloride penetration: The ingress of chlorides into concrete due to exposure to external chloride sources.Exposure temperature: The temperature of the exposure liquid while the test specimen is submerged in it.Exposure time: The time from immersion of the test specimen in the exposure liquid to profile grinding.Profile grinding: Grinding off concrete powder in thin suc-cessive layers from a test specimen using a dry process.Maturity-day: A concrete of 28 maturity-days has developed a maturity corresponding to curing for 28 days at 20 °CSurface-dry condition: Is achieved by drying the water-satu-rated test specimen with a clean cloth or similar leaving the test specimen damp but not wet. This is achieved by wetting the cloth with the liquid in which the test specimen has been immersed and then wringing it out sufficiently to absorb any liquid adhering to the surface of the specimen.5S A M P L I N GThis method requires drilled cores or cast cylinders as test specimens. They must be representative of the concreteand/or structure in question. The concrete must be hardened to minimum 28 maturity-days. At least three test specimens should be used in the test. The diameter should be at least Ø75 mm, but not less than 3 lines the maximum aggregate size. The length should be minimum 100 mm.6 METHOD OF TEST6.1PrincipleA water-saturated concrete specimen is on one plane surface exposed to water containing sodium chloride. After a specified exposure time thin layers are ground off parallel to the ex-posed face of the specimen and the chloride contant of the layers, C x, is measured. The original (initial) chloride content of the concrete, C j, is measured at a suitable depth below the exposed surface. The effective chloride transport coefficient, D e, and the boundary condition of the chloride profile at thePublished by NORDTEST Tekniikantie 12, FIN-02150 ESPOO, FINLAND Phone +358 9 455 4600 Fax +358 9 455 4272 ISSN 0283-7153Proj. 0.40x lH The first layer is omitted in the regression analysis0.258si! 0.1550.05E。

DLRO 10和DLRO 10X数字微纳吸力计说明书

DLRO 10和DLRO 10X数字微纳吸力计说明书

DLRO 10 and DLRO 10X Digital MicrohmmeterDESCRIPTIONDLRO 10 and DLRO 10X set the standards for low resistance measurement. DLRO 10 and DLRO 10X are fully automatic instruments, selecting the most suitable test current up to 10 A d.c. to measure resistance from 0.1 µΩ to 2000 Ω, on one of seven ranges.For users who desire more control over the measurement process, DLRO 10X uses a menu system controlled by a two-axis paddle to allow the user to manually select the maximum test current.DLRO 10X also adds real time download of results and on board storage for later download to a PC.Both instruments are built into a strong, lightweight case that is equally at home in the field or in the laboratory. Light enough to be worn around the neck, they are small enough to be taken into areas that were previously too small to access.DLRO 10 uses a large, bright 4 1/2 -digit LED display while DLRO 10X has a large, backlit LCD display. Normally, measurements are made with forward and reverse currents to cancel the effects of any standing voltages across the test sample.The average value is then displayed within 3 seconds, to a basic accuracy of 0.2%. DLRO 10X displays both forward and reverse measurements as well as the average of the two.DLRO 10X allows the user to set high and low pass limits, thereby enabling simple go-no-go testing.At the end of a test DLRO10X will store the test results, as well as any notes relevant to the test.To assist operator safety and ease of use, both instruments are supplied complete with a pair of duplex handspikes with 1.2 m (4 ft) leads. One of the probes is fitted with LED’s, which duplicate indicators on the instrument display indicating that all four contacts have been made, the presence of a high voltage across the load, and the presence of current flow while a load is discharging. A full range of test leads is available with probes, clamps and Kelvin clips. The instruments are supplied as standard with a Nickel Metal Hydride (NiMH) battery pack. The battery packs are inter- changeable so that an exhausted battery may be recharged using the external charger supplied while testing continues using a spare pack. Although full charging will take 4 hours, a fast charge mode allows the battery to be 90% charged within 2 1/2 hours from a 12 volt battery or from a standard 120/230 V AC supply via the supplied charger. The battery pack contains its own battery state indicator, which allows the charge-state to be monitored, even without being connected to the instrument.In addition an optional mains / line power supply, the DLRO10LPU is available. This enables the instruments to be directly powered from 90V to 264V, 50/60Hz ideal for repetitive testing applications such as manufacturing production line use.”DLRO 10X is fitted with RS232 communications that will allow results to be downloaded in real time or stored for later retrieval. Up to 700 sets of results may be stored within DLRO 10X complete with notes containing up to 200 characters which may be added using the on board keypad. These results can also be downloaded to a PC.n Auto current reversal cancels standing emfsn Protected to 600 Vn Automatically detects continuity in potential and current connectionsn Multiple operating modes including fully automaticn Alpha-numeric keypad for entering test notes (DLRO 10X)n User selectable high and low limits (DLRO 10X)n Printer output and memory (DLRO 10X)DLRO 10 AND DLRO10XDigital Microhmmeter 1981DLRO 10 AND DLRO 10XDigital MicrohmmeterMEASUREMENT MODES:A variety of measurement modes are available. Since the introductionof V2.0 firmware, Normal, Auto, Continuous and Inductive mode areavailable on both the DLRO 10 and the DLRO 10X.DLRO 10 will display the average of the measurements achievedusing forward and reverse current, while DLRO 10X displays bothindividual measurements and the average.Normal mode initiates a test by pressing the Test button on theinstrument front panel after connecting the test leads. Continuityof all four connections is checked, forward and reverse currentsare applied.Auto mode allows forward and reverse current measurements tobe made and the average displayed simply by making contact withall four probes. This mode is ideal when working with the suppliedhandspikes. Each time the probes are removed and reconnected tothe load another test will be performed without the need to pressthe test button on the instrument.Continuous mode allows repeated measurements to be madeon the same sample. Simply connect the test leads and press thetest button. The measurement is updated every 3 seconds until thecircuit is broken.Inductive mode is intended for use when measuring inductiveloads. When measuring inductive loads it is necessary to wait forthe voltage to stabilise. This means that the measurement couldtake a few seconds or several minutes. The test leads are firmlyconnected to the item to be measured and the Test button ispressed. The instrument will pass a current through the sampleand wait for the voltage to stabilise. If possible the current willbe increased. This procedure will be repeated until the voltagedetected falls into the range 15 mV to 200 mV. The instrument willthen continue to take readings, which will gradually decrease to thetrue value as the voltage stabilises further. The operator decideswhen the result is stable and presses the test button to terminatethe test. Measurement is made with forward current only.Unidirectional mode, on DLRO 10X only, applies a current in onedirection only. This does not enable any standing emfs to be negatedbut speeds up the measurement process. Test starts automaticallywhen probes are connected.APPLICATIONSThe needs for accurate low resistance measurement are wellknown and very diverse. They range through Goods Receivinginspection of components to ground bonding and welded joints.Typical applications include, but are not limited to, making d.c.resistance measurements of:n Switch and contact breaker resistancen Busbar and cable jointsn Aircraft frame bonds and static control circuitsn Integrity of welded jointsn Inter-cell connections on battery systems up to 600 V peakn Quality control of resistive componentsn Transformer and motor winding resistancen Rail and pipe bondsn Metal alloys, welds and fuse resistancen Graphite electrodes and other compositesn Wire and cable resistancen Transmitter aerial and lightning conductor bondingFEATURES AND BENEFITSn Small, lightweight and portable - can be used in tight places,reduces the need for extra long leads and two person operation.n Four terminal resistance method shows the true resistance of theitem under test.n Bright LED (DLRO 10) and LCD (DLRO 10X) displays are easilyvisible under all lighting conditions and reduce human error.n Automatically applies forward and reverse currents which cancelout any standing voltages across the sample under test.n Checks for undue noise during measurement, reducing thepossibility of recording the incorrect result.n Automatically detects continuity in P and C circuits, preventingerroneously high reading to be taken due to high resistance con-tact.n Battery module has a battery condition indicator allowing the userto check the state of spare batteries without connecting to theinstrument.n RS232 connector on the DLRO 10X allows downloading of resultsin real time or stored for later retrieval.DLRO 10 AND DLRO 10XDigital Microhmmeter Full Scale1.9999 mΩ19.999 mΩ199.99 mΩ1.9999 Ω19.999 Ω199.99 Ω1999.9 ΩResolution0.1 µΩ1 µΩ10 µΩ100 µΩ1 mΩ10 mΩ100 mΩAccuracy*±0.2% ±0.2µΩ±0.2% ±2 µΩ±0.2% ±20 µΩ±0.2% ±0.2 mΩ±0.2% ±2 mΩ±0.2% ±20 mΩ±0.2% ±0.2 ΩResistive20 mV20 mV20 mV20 mV20 mV20 mV200 mVInductiven/a20 mV200 mV200 mV200 mV200 mV200 mVResistive10 A1 A100 mA10 mA1 mA100 µA100 µAInductiven/a1 A1 A100 mA10 mA1 mA100 µAResistance ranges Test currentDLRO 10DLRO 10XMeasurement: Mode:Manual, Auto, Continuous, Inductive Manual, Auto, Continuous, Inductive,UndirectionalControl:Fully Automatic Fully Automatic/ManualSpeed:<3s for forward & reverse current and to display averageDisplay: Measurement: 4 1/2 digit seven segment LEDRange and Safety:LED indication Large backlit LCDTest Method: Single cycle reversing d.c. ratiometric measurement -average result display.Test Current: Accuracy:±10%Stability:<10 ppm per secondMaximum Lead Resistance:100 mΩ total for 10 A operation irrespective of batterycondition.Voltmeter input impedance:> 200 kΩHum rejection:Less than 1% ±20 digits additional error with 100 mV peak 50/60 Hz. on the potential leads.Warning will show if hum or noise exceeds this level.Data:Transfer:Real Time or from storage via RS232Storage:700 testsMemo Field:Up to 200 characters per test via integralalphanumeric keypadBattery: Capacity:7 Ah NiMH rechargeableLife:Typically 1000 x 10 A tests before rechargeRecharge:Via external 90 V - 260 V 50/60 Hz charger or from 12 to 15 V dc supplyCharging Rate: Standard: 2.5 hours to 90% capacity, 4 hrs for full chargeTemperature:Operation:+5 ºC to +45 ºC (41 ºF to 113 ºF) at full specification-10 ºC to +50 ºC (14 ºF to 122 ºF) at reduced accuracyStorageCo-efficient:-30 ºC to +70 ºC (-22 ºF to 158 ºF)Slow charging:<0.01% per ºC over range 5 ºC to 40 ºC (<0.006% per ºF from 4 1ºF to 104 ºF)Humidity (max):+10 ºC to +45 ºC (50 ºF to 113 ºF)Altitude (max):90% RH @ 40 ºC (104 ºF) non-condensingSafety:2000 m (6562 ft) to full safety specificationsEMC:In accordance with IEC61010-1 600 V Category III - only when DH6 leads are used.In accordance with IEC61326-1Dimensions:220 x 100 x 237 mm (8.6 x 4 x 9.5 in)Weight: 2.6 kg (5 3/4 lb.) including battery module* The accuracy stated assumes forward and reverse measurements.Inductive mode or undirectional mode will introduce an undefined error if an external EMF is present.Full scale voltsDLRO 10 AND DLRO 10XUKArchcliffe Road Dover CT17 9EN England T +44 (0) 1304 502101F +44 (0) 1304 207342******************UNITED STATES 4271 Bronze WayDallas TX 75237-1019 USA T 800 723 2861 (USA only)T +1 214 333 3201F +1 214 331 7399******************OTHER TECHNICAL SALES OFFICESValley Forge USA, College Station USA, Sydney AUSTRALIA, Täby SWEDEN, Ontario CANADA, Trappes FRANCE, Oberursel GERMANY, Aargau SWITZERLAND, Kingdom of BAHRAIN, Mumbai INDIA, Johannesburg SOUTH AFRICA, Chonburi THAILAND, Malaga SPAINRegistered to ISO 9001:2008 Cert. no. Q 09250 Registered to ISO 14001-2004 Cert. no. EMS 61597DLR10_DLRO10X_DS_en_Megger is a registered trademarkOPTIONAL MAINS / LINE POWER SUPPLY UNITThe DLRO10 and DLRO10X may also be powered from an optional mains / line power supply unit the DLRO10LPU. This unit is simply fitted to the instrument in place of the standard battery pack.When in use a red LED is illuminated when theinstrument is powered from a mains / line power supplyThe DLRO10X is seen here fitted with the optional DLRO10LPUIdeal for repetitive testing applications such as manufacturing production line use。

垂直风速标准差 英文简称

垂直风速标准差 英文简称

垂直风速标准差英文简称Vertical Wind Speed Standard DeviationThe understanding of atmospheric turbulence and its characteristics is of paramount importance in various fields, such as aviation, wind energy, and environmental studies. One crucial parameter that provides valuable insights into the nature of turbulence is the vertical wind speed standard deviation. This metric serves as a reliable indicator of the intensity and fluctuations of vertical air movements, allowing researchers and professionals to make informed decisions and mitigate potential risks.Vertical wind speed standard deviation, often denoted as σw, is a statistical measure that quantifies the dispersion or variability of vertical wind speeds around their mean value. It is calculated by taking the square root of the variance of the vertical wind speed measurements. The variance, in turn, is determined by summing the squared deviations of each measurement from the mean and dividing the result by the number of observations.The significance of vertical wind speed standard deviation lies in its ability to characterize the turbulence intensity within the atmosphericboundary layer. In this layer, which extends from the Earth's surface to the point where the wind speed becomes constant with height, the interactions between the surface and the overlying air create complex wind patterns and eddies. These turbulent fluctuations can have a profound impact on various processes, including aircraft stability, wind turbine performance, and the dispersion of pollutants.In the context of aviation, vertical wind speed standard deviation is particularly important for understanding the behavior of aircraft during takeoff and landing. Sudden changes in vertical wind speed can lead to significant variations in the lift generated by the aircraft's wings, potentially causing unexpected pitching or rolling movements. Pilots and air traffic controllers rely on accurate measurements of σw to anticipate and mitigate the effects of turbulence, ensuring the safety and efficiency of flight operations.Similarly, in the wind energy industry, the vertical wind speed standard deviation is a crucial parameter for the design and optimization of wind turbines. Turbulence intensity, as indicated by σw, can significantly impact the power output, structural integrity, and fatigue life of wind turbines. By understanding the local turbulence characteristics, wind farm developers can select appropriate turbine models, adjust their layout, and implement effective control strategies to maximize energy generation and minimize maintenance costs.Beyond aviation and wind energy, the vertical wind speed standard deviation also plays a crucial role in environmental studies and atmospheric modeling. Accurate measurements of σw can help researchers understand the transport and dispersion of air pollutants, the formation and evolution of clouds, and the interactions between the Earth's surface and the atmosphere. This information is essential for developing reliable weather forecasting models, designing effective air quality management strategies, and assessing the impact of climate change on local and regional scales.To measure vertical wind speed standard deviation, researchers and meteorologists typically employ specialized instruments, such as sonic anemometers or Doppler lidar systems. These devices are capable of accurately measuring the three-dimensional wind vector, including the vertical component, at high temporal and spatial resolutions. By analyzing the time series of vertical wind speed data, the standard deviation can be calculated and used to characterize the turbulence characteristics of the local environment.It is worth noting that the vertical wind speed standard deviation is not a static value but can vary significantly depending on factors such as atmospheric stability, surface roughness, and the presence of obstacles or terrain features. Diurnal and seasonal variations in atmospheric conditions can also influence the magnitude andpatterns of σw, requiring continuous monitorin g and analysis to gain a comprehensive understanding of the turbulence dynamics.In conclusion, the vertical wind speed standard deviation is a crucial parameter in the study and understanding of atmospheric turbulence. Its applications span a wide range of disciplines, from aviation and wind energy to environmental science and climate research. By accurately measuring and analyzing σw, researchers and professionals can make informed decisions, optimize operational strategies, and contribute to the advancement of our knowledge of the complex interactions within the Earth's atmosphere.。

化学需氧量 英语

化学需氧量 英语

化学需氧量英语Chemical Oxygen Demand (COD)The concept of Chemical Oxygen Demand (COD) is a crucial parameter in the field of environmental science and water quality management. COD is a measure of the amount of oxygen required to oxidize all the organic and inorganic matter in a water sample, both biodegradable and non-biodegradable. This measurement is essential in understanding the overall pollution load of water bodies and the subsequent treatment required to meet environmental standards.The importance of COD lies in its ability to provide a comprehensive understanding of the water's quality. Unlike the Biochemical Oxygen Demand (BOD) test, which only measures the amount of oxygen required for the biological breakdown of organic matter, COD encompasses a wider range of organic and inorganic compounds. This includes substances that are resistant to biological degradation, such as certain industrial chemicals, pesticides, and even some types of organic matter.The COD test is performed by adding a strong oxidizing agent, suchas potassium dichromate (K2Cr2O7), to a water sample. The oxidizing agent reacts with the organic and inorganic matter, converting them to carbon dioxide and water. The amount of oxygen consumed during this process is then measured and expressed as the COD value, typically in milligrams of oxygen per liter of water (mg/L).The COD test is widely used in various industries and applications, including municipal and industrial wastewater treatment, surface water quality monitoring, and groundwater assessment. In the wastewater treatment context, COD is a crucial parameter for determining the effectiveness of the treatment process and ensuring compliance with environmental regulations. By monitoring the COD levels, operators can optimize treatment strategies, ensure efficient removal of pollutants, and minimize the impact of effluent discharge on receiving water bodies.Furthermore, COD measurements are essential in the management of industrial processes, where the disposal of high-strength waste streams can have significant environmental consequences. Industries such as food processing, pulp and paper, and chemical manufacturing rely on COD analysis to assess the pollution load of their wastewater and implement appropriate treatment methods.In addition to its practical applications, COD measurement also playsa vital role in scientific research and environmental monitoring. Researchers use COD data to study the sources, transport, and fateof organic and inorganic pollutants in aquatic ecosystems, as well as to assess the overall health and resilience of these systems. This information is crucial for the development of effective environmental policies, conservation strategies, and sustainable resource management practices.Despite its widespread use, the COD test is not without its challenges. The method can be influenced by the presence of certain inorganic compounds, such as chlorides and nitrites, which can interfere with the oxidation process. Additionally, the COD test does not provide information on the specific nature of the organic compounds present, which can limit its usefulness in certain applications.To address these challenges, researchers and practitioners have developed various modifications and alternative methods for COD determination, such as the use of specific oxidizing agents, microbial-based assays, and advanced analytical techniques like gas chromatography-mass spectrometry (GC-MS) and liquid chromatography-mass spectrometry (LC-MS).In conclusion, the Chemical Oxygen Demand (COD) is a fundamental parameter in the field of water quality assessment and environmental management. It provides a comprehensive understanding of thepollution load in water bodies, enabling informed decision-making and the implementation of effective treatment strategies. As environmental concerns continue to be a global priority, the importance of COD monitoring and analysis will only increase, contributing to the sustainability and protection of our precious water resources.。

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2 neto-plasmons are not excited), was not considered. This is addressed in the present note.Let us suppose, to start with, that all of the single-particle composite fermion edge states at the Fermi level propagate in the reverse direction as in the Hartree models of a ν=2/3 hard edge,7,8 and compare this scenario with the accepted edge state picture of the integer quantum Hall effect2-5 in which all of the electron edge states travel in the standard direction. These two situations are shown schematically in Fig.1(a) and Fig.1(b), respectively. In Fig.1 the black areas represent con-tacts. In Fig.1(b) the arrows indicate the (standard) direction of propagation of single-particle elec-tron edge states. In Fig.1(a) the arrows show the (reverse) direction of propagation predicted by the Hartree models for the single-particle composite fermion edge states.Suppose that initially each of the two systems shown in Fig.1 is at equilibrium so that the electron electrochemical potentials of all of its four contacts are equal. Now let us increase the elec-tron electrochemical potential of contact 1 in each device slightly (and adiabatically) while keeping the electron electrochemical potentials of the other three contacts fixed. It is well established ex-perimentally (and is a consequence of the second law of thermodynamics) that this results in a net flux of electrons out of contact 1 and into the device. For the case in Fig.1(a) this also implies that there must be a net flux of composite fermions into the device from contact 1 because the transfor-mation from electrons to composite fermions is a gauge transformation and therefore preserves both charges and electric currents.Because of the direction of propagation of the electron states at the edges, in the case of Fig.1(b) the net flux of electrons from contact 1 into the device must be associated with a rise of the electron electrochemical potential µa along edge a of the device as is illustrated in the lower part of Fig.1(b). This results in an unbalanced flux of electrons flowing into the device along edge a, which is indicated by the heavy directed line in the figure. This unbalanced electron flux contin-ues on, following edge h into contact 2. On the other hand, because of the assumed direction of propagation of composite fermion edge states in Fig.1(a), the situation there is different: The net flux of composite fermions coming from contact 1 must be achieved by a rise of the composite fer-mion electrochemical potential µb* along edge b. Thus the unbalanced composite fermion flux in Fig.1(a) must flow along edge b and continue along edge c to contact 4. [Note that a net flux of composite fermions out of contact 1 would also occur if the composite fermion electrochemical po-tential along edge a in Fig.1(a) were lowered instead of that along edge b being raised. However, this way of realizing a net flux out of contact 1 in response to the change in the electrochemical potential of contact 1 would be unphysical since the composite fermions along edge a originate at contact 2, and therefore their electrochemical potential should be determined by the conditions at contact 2 and not at contact 1].Now consider a Hall resistance measurement in which contact 1 is the electron source (as in the above discussion), contact 3 is the electron drain, and contacts 2 and 4 are the Hall voltage probes which draw no net current. Experimentally (or once again as a consequence of the second law of thermodynamics) the net electron flux out of a contact increases (algebraically) when the electron electrochemical potential of the contact is raised. Therefore in order to satisfy the condi-tion that contacts 2 and 4 act as voltage probes and draw no net current in the above thought exper-iment, it is necessary to raise the electron electrochemical potential of contact 2 in Fig.1(b) and of contact 4 in Fig.1(a). That is, the Hall voltage generated in Fig.1(a) has the opposite sign to that generated in Fig.1(b).This means that the Hall voltage that is generated in a composite fermion system in which all of the single-particle composite fermion edge states propagate in the reverse direction has the opposite sign to that generated in systems in the integer quantum Hall regime. The same result is3 true for macroscopic composite fermion systems in which a majority of the branches of single-par-ticle composite fermion edge states at the Fermi level propagate in the reverse direction. This is because an edge carrying N standard and M reverse channels with M > N behaves like an edge with M − N reverse channels and no standard channels if the edge is of macroscopic length so that the channels that it carries can equilibrate, a result proved in the theory of quantum railroads.11 Thus the prediction of the Hartree theories that for a ν=2/3 edge (whether soft or hard) a ma-jority of the branches of single-particle composite fermion edge states at the Fermi energy propa-gate in the reverse direction, implies that the Hall voltage for a macroscopic ν=2/3 device should have the opposite sign to that observed in the integer quantum Hall regime. It is very well estab-lished experimentally however that the sign of the Hall voltage is the same at ν=2/3 (and at the oth-er fractional Landau level fillings) as it is in the integer quantum Hall regime.12 It is therefore evident that the predictions that the Hartree theories make about the direction of propagation of the single-particle composite fermion edge states for ν=2/3 conflict with the re-sults of d.c. transport experiments. This disagreement is also present for other Landau level filling fractions for which the composite fermion effective magnetic field is antiparallel to the true mag-netic field in the bulk of the sample. On the other hand there is no such disagreement between ex-periments and the predictions of the model of composite fermion edge states proposed in Ref. 6.I wish to thank B. L. Johnson, C. J. B. Ford and D. B. Chklovskii for interesting discussions. This work was supported by NSERC of Canada.References:1 J. K. Jain, Phys. Rev. Lett. 63, 199 (1989); Science 266, 1199 (1994).2 B. I. Halperin, Phys. Rev. B25, 2185 (1982).3 P. Streda, J. Kucera and A. H. MacDonald, Phys. Rev. Lett. 59,1973(1987).4 J. K. Jain and S. A. Kivelson, Phys. Rev. Lett. 60,1542 (1988).5 M. Büttiker, Phys. Rev. B38, 9375 (1988).6 G. Kirczenow and B. L. Johnson, Phys. Rev. B51, 17579 (1995) - download paper cond-mat/ 9502058 from the e-print archive at the www site / for legible figures; G. Kirc-zenow and B. L. Johnson, to be published in Surface Science, paper cond-mat/ 9508069 at thee-print archive at the www site /7 L. Brey, Phys. Rev. B50, 11861 (1994)8 D. B. Chklovskii, Phys. Rev. B51, 9895(1995).9 D. B. Chklovskii and B. I. Halperin, in the Proceedings of the Eleventh International Conference on the Electronic Properties of Two Dimensional Systems, Nottingham, U.K., 1995.10 R. C. Ashoori, H. L. Störmer, L. N. Pfeiffer, K. W. Baldwin, and K. West, Phys. Rev. B45, 3894 (1992).11 C. Barnes, B. L. Johnson and G. Kirczenow, Phys. Rev. Lett. 70,1159 (1993); Canadian Jour-nal of Physics 72, 559 (1994).12 See The Quantum Hall Effect, edited by R. E. Prange and S. M. Girvin, Springer Verlag, 1987.4Figure Caption:Fig.1 Schematic drawing of two Hall bars. The black areas are contacts. The arrows show the direction of propagation for single-electron edge states in the integer quantum Hall regime in Fig.1(b), and the majority direction of propagation for composite fermion single-particle edge states predicted by the Hartree models at ν=2/3 in Fig.1(a). The heavy directed curves indicate the path of the unbalanced flux of electrons (Fig.1(b)) and composite fermions (Fig.1(a)) when the electron electrochemical potential of contact 1 is increased. The plots at the bottom show schemat-ically the electron (Fig.1(b)) and composite fermion Hartree (Fig.1(a)) Landau level structure along the dashed lines ab in the respective Hall bars depicted above and the corresponding electron and composite fermion edge electrochemical potentials µ and µ*, respectively.。

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