1) dry season
枯水期，旱季
2) dry season
枯水季
1.
Study on water allocation in dry season in estuarial areas along main stem of Yangtze River;
长江干流河口地区枯水季水量分配研究
4) dry season
枯水期
1.
Various forms of inorganic nitrogen(N) of surface water were investigated in the Ganjiang River catchments during January(dry season) and July(flood season),2006.
于2006年1月和7月对赣江流域地表水进行了系统采集,分析研究了水体中各形态无机氮分布特征,结果表明,赣江水体中主要的氮素形式是NO3--N,枯水期赣江流域NO3--N、DIN从上游至下游呈明显的上升趋势,NH4+-N变化不明显。
2.
We thought,at the beginning of high water season,the water quality obviously surpassed the end of dry season with the middle level eutrophic status in Shuanglong-lake,while at the end of dry season,it was at light eutrophic status.
对双龙湖枯、丰水期交替期各项水质指标TN、TP、CODm n、Ch la、透明度、浊度等指标进行监测分析,运用富营养化综合评价法对双龙湖营养状态进行评价,认为双龙湖丰水期初期水质优于枯水期末期,处于中营养化水平,枯水期末期处于轻富营养状态。
3.
Introducing the application of auto matic hydrological information acq uisition system(thereaftersystem)in water resources optimizing configuration of Shanmei Reservoir durin g dry season,the author holds some problems of un -completion in parame ters and functions set in system.
通过水文自动测报系统在山美水库枯水期水资源优化配置应用的分析,认为系统还存在参数、功能不全等问题,通过分析这些问题,并给出相应解决问题的方法,使水文自动测报系统的作用在效益最大化、以供水定发电、水量动态平衡等原则基础上的枯水期水资源调度中得到了体现。
5) drought period
枯水期
1.
The climate characteristics and the incoming flow distribution law during drought period were analyzed in research basin.
在分析研究流域气候特征及枯季径流来水规律的基础上,用水文气象方法和水文方法分别建立了枯水期月径流预报模型。
2.
This paper firstly determines the Three Gorges monthly water flow output of dif-ferent hydrological years by using compensative scheduling calculation, taking into consideration of natural enhancement of inflows to the Three Gorges reservoir during drought period due to joint operation of main reservoirs located on the upper reaches of the Yangtze River.
考虑长江上游干支流主要水电站水库对三峡枯水期流量的自然提高作用下，确定三峡水电站不同水文年枯水期逐月水流平均出力的时间分布；并在三峡确定的供电范围和电力电量分配方案条件下，通过华中、华东系统的电力电量平衡，研究了二大区系统对三峡电站枯水期电力电量的吸收利用情况；最后根据平衡结果，以充分利用三峡电力电量为原则，提出三峡枯水期电力电量的经济合理分配建议。
6) low-flow period
枯水期
1.
Sulfur isotopic compositions of Wujiang River water in Guizhou Province during low-flow period;
贵州乌江水系枯水期河水硫同位素组成研究
补充资料：枯水位
地面水流近于枯竭，主要依靠地下水补给而维持比较稳定且较低的水位。多产生于流域内少雨季节。也有依据历年观测资料确定一上限，低于此限的水位即称枯水位。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条