1) water level during dry period
枯水期水位
2) 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。
3) 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。
4) 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
5) low water period
枯水期
1.
Hydraulic factors and water quality of low water period in 2006 were computed in study area.
根据平原河网在不同水文时期关注的目标,应用建立的水流水质计算模型,对研究区历史发生的5场洪水水流进行了验证,并对现状枯水期水流和水质进行了计算。
2.
The main two contaminations,namely(NH~+_4-N) and TP,are simulated on the platform of MapInfo and Delft3D in the Qiantang River at the low water period,to analyze its space-time diversity.
确立基于可视化技术的污染物水环境模拟技术框架,建立水环境空间模型,基于MapInfo和Delft3D平台对钱塘江枯水期主要污染物氨氮(NH4+-N)、总磷(TP)进行模拟,对其时空变化规律进行分析。
3.
Functions and flow characteristics are different in plain river networks by flood and low water period,leading function is demanded in flood period while water supply function is demanded in low water period.
平原河网在洪水期注重行洪要求,在枯水期要提供一定的用水功能,不同时期的水流变化具有不同的特点,需要了解水流的变化规律以调控河网水位。
6) dry seasons
枯水期
1.
Due to the large proportion of small sized hydro power in Qingyuan power system as well as the far location from load center,the operation mode is far different during the raining seasons and dry seasons.
由于清远地理位置的特殊性 ,小水电比例较大且远离负荷中心 ,使得清远电网丰、枯水期电网运行方式有很大的不同。
2.
The reasons and mechanism of water intaking difficulty in North Nenjiang Diversion Project during dry seasons were analyzed.
探讨了北部引嫩工程（以下简称“北引”）枯水期出现引水危机的成因和机理。
补充资料：地下水水位观测(见水位观测)
地下水水位观测(见水位观测)
d ixiashui shuiwei guanee地下水水位观测见水位观测。
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