地下水补给量

同时还会减少地下水补给量，升高地下水补给温度，引起地下水水化学作用发生变化。

At the same time , the increasing temperature can also reduce groundwater recharge , elevate groundwater recharge temperature , and causes the change of groundwater hydrochemistry .

毛管水上升高度和消耗的水量与时间均呈现幂函数关系，毛管水上升高度与地下水补给量呈现明显的线性关系。

There was an obvious linear function relationship between the height of upward capillary water and groundwater recharge quantity and power function relationship between them and time .

绿化是增加地下水补给量的有效方法。

It is the valid method to add supply to underwater by afforesting .

应用同位素氚预测地下水补给量

Application of isotopic TRITUM (￣ 3h ) method to predict underground water supply amount

研究雨水入渗、提高雨水的入渗效率是充分利用洪水资源，增加地下水补给量的重要途径。

Studying precipitation infiltration and raising precipitation efficiency are very important approaches for better using flood water and recharging ground water .

研究结果表明，城市扩展是导致地下水补给量减少的主要原因之一，研究结果验证前人的科学观点。

The result expresses : it is a science standpoint that urban expansion is one of the main reasons to cause the decreasing of supply to groundwater .

本文主要通过对降水入渗机理、影响水入渗的因素、降水入渗补给量计算的研究，分析降水量与地下水补给量的关系。

The article analyzes the relationship between precipitation and groundwater replenishment by study the precipitation infiltration mechanism , factors that effect water infiltration and the calculation of precipitation infiltration replenishment .

作物产量水平的提高，在直接消耗大量水资源和土壤水分的同时，也使农田蒸散发加强，从而造成地表径流量和地下水补给量的减少。

The level increase of crop output directly consumed a great lot of water resources and soil water , simultaneously had farmland evapotranspiration strengthened , and also brought about surface runoff and groundwater recharge decreasing .

通过对封丘县历年粮食产量、降水量、引黄灌溉水量、地下水补给量等资料计算，初步估算出封丘地区粮食生产水分利用效率。

The change of water use efficiency over the years was calculated from the long term data of crop yields , precipitation , the amount of irrigation water diverted from the Yellow River or pumped wells and replenishing water from ground water in Fengqiu county .

分析了新疆平原区地下水补给量、排泄量和可开采量评价的误差来源，提出了减少评价误差的措施：一是地下水动态监测和水运行测量统计是实现逐步逼近地下水资源量的最有效方法；

By analyses of error sources of groundwater recharge , discharge and groundwater quantity exploitable , a few measures of reducing evaluation errors are proposed : ( 1 ) Dynamic monitoring of groundwater and recording of water use volume are the most effective way of estimating the actual groundwater resources ;

水源地地下水综合补给量频率分析的方法

Method of Frequency Analyses for Groundwater Comprehensive Recharge in Well Field

用同位素测井技术确定地下水侧向补给量

Determination of lateral groundwater recharge using single well techniques of a radioactive isotope

运用该模型，对各种条件下的地下水补给资源量、开采资源量进行了评价和开采潜力分析；

Then the recharge resources , allowable withdrawal and potential capacity of groundwater are estimated by using the model .

不同岩性土壤的毛细上升过程，毛细上升高度与时间，地下水累计补给量与时间的关系有所区别。

When the soil lithology changed , the relationship of capillary rise height and time and the total groundwater recharge were different .

蓄水后，在库水范围内白河侧渗底渗量增大，增大了浅层地下水的补给量，地下水动储量增大，大大缓解了市中心城区的缺水现状；

The increase of groundwater dynamic storage capacity in aquifer alleviates the intense lack of water supply in the center area of the City .

在水分耗散途经上看，晚稻中早期深灌将增加了地下水的补给量，相反，浅灌增加了空中水蒸气补给量。

Seen from water consumption way , deep-water irrigation in mid - early term of late rice increased the supply of underground water . Just on the contrary , shallow-water irrigation increased the supply of vapor in atmosphere .

在定义了水文地质参数盲数、未确知风险等基本概念的基础上，尝试性地提出了盲信息下地下水资源补给量计算模型和允许开采量的未确知风险分析方法。

Based on the definitions of hydrogeological parameter blind number and unascertained risk , a model for calculation of groundwater supply according to the blind information is established and a new method for groundwater allowable withdrawal evaluation is proposed .

地下水入渗补给量是重要的水文地质参数。

Groundwater recharge is an important parameter in hydrogeology .

惰性气体法测定地下水入渗补给量

A New Method for Determining Groundwater Recharge : the Dissolved Inert Gases Method

地下水补给与开采量对降水变化响应特征：以京津以南河北平原为例

Responses of Groundwater Recharge and Pumpage to Change in Precipitation in Hebei Plain

第三阶段应实现总需水量低于地下水系统补给资源量，使数十年超采造成的储存资源亏空逐年得以偿还。

In the third step , the total water requirement should be less than the renewable resources to compensate for the loss of storage resources due to the exploitation in the previous steps .

由于地下水的各项补给量是变化的，因此恢复补给历史、评估补给强度变化是比较困难的。

Because of large spatial and temporal variation , the direct measurement of groundwater recharge rate is hardly possible , so it is very difficult to reconstruct the groundwater recharge history and estimate the changes of recharge rate .

降水构成、温度和地表植被的改变可使地下水补给对降水量的响应增强或削弱，甚至导致地下水补给与年降水量变化在某些时段呈现相反的趋势。

In the other words , temperature and vegetation variation may increase or decrease the responses of groundwater recharge to yearly rainfall . At some times , groundwater recharge could have an opposite trend to that of yearly rainfall . 3 .

本文根据大量室内外的试验观测资料，探讨了浅层地下水入渗补给量的形成和分布规律，其成果有助于干旱、半干旱地区地下水资源评价。

Based on a large amount of laboratory and in-situ testing and observation data , this paper discusses the law of formation and distribution of shallow groundwater infiltration recharge . The result will be beneficial to the assessment of groundwater resource in arid and semi-arid regions .

运用模型确定地下水多年平均补给资源量和可开采资源评价；

Groundwater resources and safe yield are evaluated using the model .

地下水对湖泊的补给量与沙漠地区的蒸发和降水没有关系。

The amount of groundwater recharge performed no apparent relationship between evaporation and precipitation in desert .

计算结果表明，降雨入渗和河渠渗漏补给地下水分别占总补给量的50%和44%。

The study results demonstrate that precipitation recharge amount and river flow infiltration amount are 50 and 44 percent of the total water recharge amount , respectively .

本文介绍了土壤水分通量法的原理，定位通量法在估算田间土壤非饱和导水率、地下水的入渗补给量和腾发量等方面的应用。

This paper presents the principle of soil water flux approaches ( Zero Flux Plane Method , Fixed Plane Flux Method and Surface Plane Flux Method ) .

由于绿洲的农业灌溉较大程度的依赖开采地下水，地下水的补给量远远无法弥补开采量留下的缺口，因此地下水埋深随着开采量的逐年增加直线下降。

The agricultural irrigation in oasis depends on exploration of ground water , but groundwater Replenishment cannot be balanced the gap made by exploration . The buried depth linear decrease with increasing exploration .

根据数值模型计算的结果，全区地下水多年平均补给资源量为6795.82×104m3/a，大气降水入渗量占总补给量的78%；

According to the calculating result of digital model , the quantity of groundwater supplies is 6795.82 × 104m3 / a , the quantity of atmosphere precipitation soak declines have 78 % of the total replenishment quantity ;