On the basis of information from the project ＂Land-surface Processes and their Experimental Study on the Chinese Loess Plateau＂, we analyzed differences in land-surface water and heat processes during the main dry a...On the basis of information from the project ＂Land-surface Processes and their Experimental Study on the Chinese Loess Plateau＂, we analyzed differences in land-surface water and heat processes during the main dry and wet periods of the semiarid grassland growing season in Yuzhong County, as well as the influences of these environmental factors. Studies have shown that there are significant differences in changes of land-surface temperature and humidity during dry and wet periods. Daily average normalized temperature has an overall vertical distribution of ＂forward tilting＂ and ＂backward tilting＂ during dry and wet periods, respectively. During the dry period, shallow soil above 20-cm depth is the active temperature layer. The heat transfer rate in soil is obviously different during dry and wet periods. During the dry period, the ratio of sensible heat flux to net radiation （H/Rn） and the value of latent heat flux to net radiation （LE/Rn） have a linear relationship with 5-cm soil temperature; during the wet period, these have a nonlinear relationship with 5-cm soil temperature, and soil temperature of 16℃ is the critical temperature for changes in the land-surface water and heat exchange trend on a daily scale. During the dry period, H/Rn and LE/Rn have a linear relationship with soil water content. During the wet period, these have a nonlinear relationship with 5-cm soil water content, and 0.21 m^3 m^-3 is the critical point for changes in the land-surface water and heat exchange trend at daily scale. During the dry period, for vapor pressure deficit less than 0.7 kPa, H/Rn rises with increased vapor pressure deficit, whereas LEIRn decreases with that increase. When that deficit is greater than 0.7 kPa, both H/Rn and LE/Rn tend to be constant. During the wet period, H/Rn increases with the vapor pressure deficit, whereas LE/Rn decreases. The above characteristics directly reflect the effect of differences in land-surface environmental factors during land-surface water and heat exchange processes, and indirectly reflect the influences of cloud precipitation processes on those processes.展开更多
A new air-water dual source heat pump water heater with heat recovery is proposed.The heat pump system can heat water by using a single air source,a single water source,or air-water dual sources.The water is first pre...A new air-water dual source heat pump water heater with heat recovery is proposed.The heat pump system can heat water by using a single air source,a single water source,or air-water dual sources.The water is first pre-heated by waste hot water,then heated by the heat pump.Waste heat is recovered by first preheating the cold water and as water source of the heat pump.According to the correlated formulas of the coefficient of performance of air-source heat pump and water-source heat pump,and the gain coefficient of heat recovery-preheater,the formulas for the coefficient of performance of heat pump in six operating modes are obtained by using the dimensionless correspondence analysis method.The system characteristics of heat absorption and release associated with the heat recovery-preheater are analyzed at different working conditions.The developed approaches can provide reference for the optimization of the operating modes and parameters.The results of analysis and experiments show that the coefficient of performance of the device can reach 4-5.5 in winter,twice as much as air source heat pump water heater.The utilization of waste heat in the proposed system is higher than that in the system which only uses waste water to preheating or as heat source.Thus,the effect of energy saving of the new system is obvious.On the other hand,the dimensionless correspondence analysis method is introduced to performance analysis of the heat pump,which also has theoretical significance and practical value.展开更多
为了探索不同冬灌定额和地表覆盖模式对棉田水热盐的影响,该文设置了冬灌裸地(winter irrigation with bare land,WIB)、冬灌留秆(winter irrigation with high cotton stubble,WICS)、冬灌玉米秸秆覆盖(winter irrigation with corn st...为了探索不同冬灌定额和地表覆盖模式对棉田水热盐的影响,该文设置了冬灌裸地(winter irrigation with bare land,WIB)、冬灌留秆(winter irrigation with high cotton stubble,WICS)、冬灌玉米秸秆覆盖(winter irrigation with corn straw mulching,WICM)、免冬灌裸地(no winter irrigation with bare land,NWIB)、免冬灌留秆(no winter irrigation with high cotton stubble,NWICS)和免冬灌玉米秸秆覆盖(no winter irrigation with corn straw mulching,NWICM)6个处理。经过2013-11-15-2014-04-04和2014-11-15-2015-04-04冬季大田试验,得到:灌水和地表覆盖可以平抑土壤温度的变幅,免冬灌或冬灌条件下,温度变异幅度均为裸地>留秆>玉米秸秆覆盖。玉米秸秆覆盖更有利于土壤水分保持,WICM土壤储水量比WIB和WICS分别多29.10%和10.36%,NWICM土壤储水量比NWIB和NWICS分别多14.97%和2.21%,经过两年冻融过程NWIB、NWICS和NWICM 0~100 cm土壤储水量平均减少了18.32、7.36和2.62 mm。(免)冬灌0~30 cm土壤含盐量均为裸地>留秆>玉米秸秆覆盖;0~100 cm土壤范围冬灌盐分淋洗率为玉米秸秆覆盖(34.86%)>留秆(15.82%)>裸地(7.26%);免冬灌0~100cm积盐率为裸地(10.11%)>留秆(7.96%)>玉米秸秆覆盖(3.01%)。研究结果可为南疆冬季休闲期棉田土壤水热盐调控提供科学依据。展开更多
基金supported by the National Basic Research Program of China(Grant No.2013CB430206,2012CB955304)National Natural Science Foundation of China(Grant Nos.41075008,40830957,41275118)+2 种基金China Postdoctoral Science Special Foundation(Grant No.2013T60901)China Postdoctoral Science Foundation(Grant No.20110490854)the Ten Talents Program of Gansu Meteorology Bureau
文摘On the basis of information from the project ＂Land-surface Processes and their Experimental Study on the Chinese Loess Plateau＂, we analyzed differences in land-surface water and heat processes during the main dry and wet periods of the semiarid grassland growing season in Yuzhong County, as well as the influences of these environmental factors. Studies have shown that there are significant differences in changes of land-surface temperature and humidity during dry and wet periods. Daily average normalized temperature has an overall vertical distribution of ＂forward tilting＂ and ＂backward tilting＂ during dry and wet periods, respectively. During the dry period, shallow soil above 20-cm depth is the active temperature layer. The heat transfer rate in soil is obviously different during dry and wet periods. During the dry period, the ratio of sensible heat flux to net radiation （H/Rn） and the value of latent heat flux to net radiation （LE/Rn） have a linear relationship with 5-cm soil temperature; during the wet period, these have a nonlinear relationship with 5-cm soil temperature, and soil temperature of 16℃ is the critical temperature for changes in the land-surface water and heat exchange trend on a daily scale. During the dry period, H/Rn and LE/Rn have a linear relationship with soil water content. During the wet period, these have a nonlinear relationship with 5-cm soil water content, and 0.21 m^3 m^-3 is the critical point for changes in the land-surface water and heat exchange trend at daily scale. During the dry period, for vapor pressure deficit less than 0.7 kPa, H/Rn rises with increased vapor pressure deficit, whereas LEIRn decreases with that increase. When that deficit is greater than 0.7 kPa, both H/Rn and LE/Rn tend to be constant. During the wet period, H/Rn increases with the vapor pressure deficit, whereas LE/Rn decreases. The above characteristics directly reflect the effect of differences in land-surface environmental factors during land-surface water and heat exchange processes, and indirectly reflect the influences of cloud precipitation processes on those processes.
基金supported by the National Natural Science Foundation of China (Grant No. 51076147)
文摘A new air-water dual source heat pump water heater with heat recovery is proposed.The heat pump system can heat water by using a single air source,a single water source,or air-water dual sources.The water is first pre-heated by waste hot water,then heated by the heat pump.Waste heat is recovered by first preheating the cold water and as water source of the heat pump.According to the correlated formulas of the coefficient of performance of air-source heat pump and water-source heat pump,and the gain coefficient of heat recovery-preheater,the formulas for the coefficient of performance of heat pump in six operating modes are obtained by using the dimensionless correspondence analysis method.The system characteristics of heat absorption and release associated with the heat recovery-preheater are analyzed at different working conditions.The developed approaches can provide reference for the optimization of the operating modes and parameters.The results of analysis and experiments show that the coefficient of performance of the device can reach 4-5.5 in winter,twice as much as air source heat pump water heater.The utilization of waste heat in the proposed system is higher than that in the system which only uses waste water to preheating or as heat source.Thus,the effect of energy saving of the new system is obvious.On the other hand,the dimensionless correspondence analysis method is introduced to performance analysis of the heat pump,which also has theoretical significance and practical value.
文摘为了探索不同冬灌定额和地表覆盖模式对棉田水热盐的影响,该文设置了冬灌裸地(winter irrigation with bare land,WIB)、冬灌留秆(winter irrigation with high cotton stubble,WICS)、冬灌玉米秸秆覆盖(winter irrigation with corn straw mulching,WICM)、免冬灌裸地(no winter irrigation with bare land,NWIB)、免冬灌留秆(no winter irrigation with high cotton stubble,NWICS)和免冬灌玉米秸秆覆盖(no winter irrigation with corn straw mulching,NWICM)6个处理。经过2013-11-15-2014-04-04和2014-11-15-2015-04-04冬季大田试验,得到:灌水和地表覆盖可以平抑土壤温度的变幅,免冬灌或冬灌条件下,温度变异幅度均为裸地>留秆>玉米秸秆覆盖。玉米秸秆覆盖更有利于土壤水分保持,WICM土壤储水量比WIB和WICS分别多29.10%和10.36%,NWICM土壤储水量比NWIB和NWICS分别多14.97%和2.21%,经过两年冻融过程NWIB、NWICS和NWICM 0~100 cm土壤储水量平均减少了18.32、7.36和2.62 mm。(免)冬灌0~30 cm土壤含盐量均为裸地>留秆>玉米秸秆覆盖;0~100 cm土壤范围冬灌盐分淋洗率为玉米秸秆覆盖(34.86%)>留秆(15.82%)>裸地(7.26%);免冬灌0~100cm积盐率为裸地(10.11%)>留秆(7.96%)>玉米秸秆覆盖(3.01%)。研究结果可为南疆冬季休闲期棉田土壤水热盐调控提供科学依据。
文摘为准确地评价江苏徐州地区的太阳能资源及太阳能热水系统的应用效益,建立了太阳能建筑应用测评试验系统,通过测试环境温度、太阳辐照量、集热器进水出水温度、水箱进水温度、水箱热水及出水温度、出水流量等参数,分析了太阳能热水系统的集热效率和工程应用效益.测试结果表明,徐州地区具有良好的太阳能资源,太阳能热水试验系统的集热效率达到50%以上;太阳能热水作为生活热水和采暖系统热源具有良好的经济效益,在徐州市某示范工程应用中的计算投资回收期为3.2 a.
