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多年调节水库兴利库容的求解方法 被引量:2
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作者 李景玉 孙德树 《东北水利水电》 2005年第7期36-37,共2页
用基于数理统计理论的“合成总库容法”进行多年调节水库兴利库容计算时,将水库损失量列入其调节水量系列,并参与多年库容及年库容的调节计算,能解决设计供水期难于确定的问题;通过成果的逐步迭代演算,可使各项分析指标收缩于理论值,成... 用基于数理统计理论的“合成总库容法”进行多年调节水库兴利库容计算时,将水库损失量列入其调节水量系列,并参与多年库容及年库容的调节计算,能解决设计供水期难于确定的问题;通过成果的逐步迭代演算,可使各项分析指标收缩于理论值,成果更具说服力。 展开更多
关键词 来水量系列 调节水量系列:供水保证率 水库损失量 迭代逼近
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关于正确界定水库取水量的探讨
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作者 宋翠萍 《黑龙江水利科技》 2007年第3期152-152,共1页
为了保证正常兴利供水的需要,水库调度运行中均要计入一定的水库损失量,而这一损失水量也是直接从江河取蓄的,在运行当中虽已损耗,但也应计入取水量,这也符合法律的规定。
关键词 水库 正常供水量 水库损失量 取水量
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水库灌溉供水兴利调节计算
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作者 樊培培 《大科技》 2013年第18期204-205,共2页
近年来地表水用来农田灌溉显得走向缺渴之势,因此在农田灌溉设计中,供水计算是显得十分重要,现在就水库灌溉供水兴利调节计算加以分析,我们在灌溉时要考虑年、灌溉期径流测值及经验频率要与设计值相近等问题。对应的我们就应该找一... 近年来地表水用来农田灌溉显得走向缺渴之势,因此在农田灌溉设计中,供水计算是显得十分重要,现在就水库灌溉供水兴利调节计算加以分析,我们在灌溉时要考虑年、灌溉期径流测值及经验频率要与设计值相近等问题。对应的我们就应该找一些计算相应的方法,例如:供水兴利用的水和水库的损失量、渗漏损失、其他损失等。兴类调节计算的类型,兴类调节计算的内容等。因此我们在水库供水兴利调节计算采取了方法。 展开更多
关键词 水库损失量 渗漏损失 其他损失 兴利调节计算的类型
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Evapotranspiration and humidity variations in response to land cover conversions in the Three Gorges Reservoir Region 被引量:3
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作者 DENG Hua SHAO Jing-an 《Journal of Mountain Science》 SCIE CSCD 2018年第3期590-605,共16页
A new land cover classification system was established for the Three Gorges Reservoir Region(TGRR) after considering the continuity of inundation and the natural characteristics of land cover. The potential evapotrans... A new land cover classification system was established for the Three Gorges Reservoir Region(TGRR) after considering the continuity of inundation and the natural characteristics of land cover. The potential evapotranspiration(PET) was predicted using a modified Penman-Monteith(P-M) model. The region's ratio of precipitation to evapotranspiration was calculated as the humidity index(HI). The data obtained was used to analyze climatic responses to land cover conversions from the perspectives of evapotranspiration and humidity variations. The results show that, from 1997 to 2009, the average annual PET increased in the early years and decreased later. In terms of overall spatial distribution, a significant reciprocal relationship appeared between annual PET and annual HI. In 1997,the annual PET was higher in the lower reaches than in the upper reaches of the TGRR, but the areas with high PET shifted substantially westward by 2003. The annual PET continued to increase in 2006, but the areas with high PET shrank by 2009. In contrast, the annual HI showed varying degrees of localized spatial variability. Over the three periods, the dominantforms of land cover conversions occurred from evergreen cover to seasonal green cover, from seasonal green cover to evergreen cover, and from seasonal green cover to seasonally inundated areas, respectively. These accounted for 48.0%, 38.4%, and 23.8% of the total areas of converted land covers in the three periods, respectively. During the period between 1997 and 2003, the main forms of land cover conversions resulted in both positive and negative growths in the average annual PET, while all of them pushed down the average annual HI. From 2003 to 2006, the reservoir region experienced neither a decrease in the annual PET nor an increase in the annual HI. The period between 2006 and 2009 saw a consistent downward trend in the annual PET and a consistent upward trend in the annual HI. 展开更多
关键词 Land cover EVAPOTRANSPIRATION Humidity variations RESPONSE Three Gorges Reservoir Region
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