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influent seepage
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  “influent seepage”译为未确定词的双语例句
     The Q3al, Q4eol and basement groundwater flow subsystems receive the influent seepage recharge from the meteoric water, and then discharge at the eastern edge of Q3al.
     Q3al、Q4eol及基岩潜水流动子系统都接受大气降水入渗补给,最终通过Q3al的东侧边界排入黄河.
短句来源
     The Influent Seepage Prevention Measures ofChannels in Heilongjiang Province
     黑龙江省渠道防渗措施
短句来源
     Influence of Rainfall Influent Seepage in Relation to Unsaturated Soil Slope Stability
     降雨入渗对非饱和土边坡稳定性的影响
短句来源
     To account the characters of Huanglashi landslide and factor influencing its stability, and based on the analysis of law of slope runoff and influent seepage in landslide area, the arrangement principle and structure mode of surface drainage ditch was introduced in this paper.
     本文根据黄腊石滑坡特征及其稳定性影响因素,滑坡区坡面径流及入渗规律的分析,介绍了地表排水沟的布置原则和结构形式。
短句来源
     (3) in the north basin, groundwater gets water from surface water through irrigation in agricultural land or gets water from river influent seepage through riverbed.
     在农灌区引河水通过田间入渗补给地下水。 (3)北部盆地,在金塔灌区,地下水主要接受引水灌溉入渗补给;
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  相似匹配句对
     The Influent Seepage Prevention Measures ofChannels in Heilongjiang Province
     黑龙江省渠道防渗措施
短句来源
     Influence of Rainfall Influent Seepage in Relation to Unsaturated Soil Slope Stability
     降雨入渗对非饱和土边坡稳定性的影响
短句来源
     it is studied with the seepage theory.
     2.分析了非饱和土的土水势理论、广义达西定律。
短句来源
     Free Seepage and Its Application
     自由入渗及其应用
短句来源
     THE INFLUENT AND EARTHQUAKES IN XINFENGJIANG RESERVOIR
     渗流与新丰江水库地震
短句来源
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  influent seepage
The complicated process of pollutant spread was modeled as an aggregate of four simpler models such as overland water flow, influent seepage, pollutants transport with surface runoff, and pollutant deposition (accumulation) on the land surface.
      


Weihe river,the largest tributary of Yellow river,is the main trunk river of river system in thecentral Shaanxi Plain.Weihe river plain is situated in the middle sector , Shaanxi province.It was resulting from longevolution of Weihe river system. It is a Cenozoic graben basic with considerable thich Cenozoicdeposits. The south and north borders are respectively bounded by Qinling Mountains and NorthMountains,Which extends about 300km in length from Baoji on the west to Tongguan on east,Shaanxi province where...

Weihe river,the largest tributary of Yellow river,is the main trunk river of river system in thecentral Shaanxi Plain.Weihe river plain is situated in the middle sector , Shaanxi province.It was resulting from longevolution of Weihe river system. It is a Cenozoic graben basic with considerable thich Cenozoicdeposits. The south and north borders are respectively bounded by Qinling Mountains and NorthMountains,Which extends about 300km in length from Baoji on the west to Tongguan on east,Shaanxi province where it meet Yellow river.Weihe river has an asymmetric drainage.Its north bank tributaries present a dendritic drainage,whereas south tributaries a featherllke drainage.Baiyang source region of water is located at the flood plain-terrace I on the south bank of Weiheriver, near the Linghe- Weihe rivers junction at Baiyang country in Weinan county , covering an areaabout 10km ̄2. It is a source region of water of polylaminate texture consisting of quaternary alluvionsand lake deposits, containg a phreatic water,a shallow,a middle and a deep confined water four aquifers。Phreatic water is maily supplied by lateral influent seepage of river,and infiltration ofprecipitated water.Being exploited,it is mainly supplied by lateral influent seepage of river and run-off.Confined water is mainly supplied by underground water flow from west side of explorationregion,As phreatic table is a little higher than shallow confined water, and middle confined waterhigner than deep confined water, there is an overwash relationship between them,Shallow confinedwater and phreatic water in some section of seurce region of water turn into saline water.It resultfrom gelolgical environment and hydrogeochemical environment characters of the storage andmigration of underground water at the source region of water。Feeding water from Weihe river makes up abeut 1/2 of feeding phreatic water at the Baiyangseurce region of water,Water-bearing strata have a better pormeabiling,and water exchange is bettertoo,The water preduction of a single well is more than 5 0 00m ̄3/d.Middle and deep confined waterwas buried at a deeper depth,with feeder channel being longer,and the age of underground waterbeing more than 4 000-8000 years.B.P.

白杨水源地座落在渭河下游重镇——渭南市西北约5km处,为谓河冲积平原的一部分。区内第四纪松散堆积物巨厚,地形平坦,降水充沛,地表水丰富,为地下水储存提供了良好的空间。按含水介质的埋藏条件可划分为潜水、浅层承压水、中层承压水和深层承压水4个含水岩组。为了进一步研究地下水的补给形成机制、储存运移过程、排泄开采条件,本文结合环境同位素(包括 ̄(14)C、 ̄(13)C、 ̄3H、D和 ̄(18)O)对水源地地下水年龄、地下水运动速率以及一些水文地质参数进行研究和探讨。而同位素测定表明:水源地潜水为现代水, ̄3H含量较高,河水补给量占1/2左右;中、深层承压水补给途径较远, ̄(14)C年龄分别在距今0.4-0.5Ma和0.8-0.9Ma左右;δD和δ ̄(18)O值变化不大,说明它们主要来源于大气降水补给。

The authors discuss the vertical water migration mechanism in the aeratedzone and offer a simple method by using the Poisson Random Model to predict the dynamic changes of phreatic level. The features of the method are to take the areatedzone between surface and groundwater tables as a complete system and take the Poisson Distribution Function as a responding function of the system as well as water loss which is caused by rainfall and evaporation in the ground as a input of the system during the calculation...

The authors discuss the vertical water migration mechanism in the aeratedzone and offer a simple method by using the Poisson Random Model to predict the dynamic changes of phreatic level. The features of the method are to take the areatedzone between surface and groundwater tables as a complete system and take the Poisson Distribution Function as a responding function of the system as well as water loss which is caused by rainfall and evaporation in the ground as a input of the system during the calculation of the dynamic changes of phreatic level. The Poisson Distribution Function belongs to a function of discrete stochastic distribution and is similar to the distributed properties of the phreatic level observation data with the discrete time-continuous state.Additionally,the areatedzone falls to some water-storage bodies and water moving in the water-storage bodies obeys the regularity of the Poisson Distribution. The input of system and water migration in areatedzone have same dissemination regularity.Therefore,the performance could be really reflected by the output of the system i.e.dynamic phreatic level. By using the model to predict dynamic changes of phreatic level,the relationship between the atmospheric water,phreatic evaporation and level can be understood correctly. It is suitable to use in plain regions with low angular slope where the water migration in the areatedzone belongs to influent seepage-evaporation type.

泊松模型预测潜水位动态变化陈锁忠,陶芸江苏省地质环境监测总站,南京,210049关键词:泊松模型,潜水位,动态预测,江苏盐城UsingthePoissonModeltoPredictDynamicChangesofthePhreaticLevel¥C...

The drainage is a common measure of landslide administer. Suitable drainage measure can effectively prevent landslide activity, but the effect is not well if unsuitable. To account the characters of Huanglashi landslide and factor influencing its stability, and based on the analysis of law of slope runoff and influent seepage in landslide area, the arrangement principle and structure mode of surface drainage ditch was introduced in this paper.

排水是常用的滑坡治理措施,合理的排水措施可有效地防止滑坡活动,布置不当则效果不大。本文根据黄腊石滑坡特征及其稳定性影响因素,滑坡区坡面径流及入渗规律的分析,介绍了地表排水沟的布置原则和结构形式。

 
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