地下水资源量

  • 网络ground water resources amount;quantity of groundwater resources
地下水资源量地下水资源量
  1. 费县地下水资源量的估算与分析

    Estimation & Analysis of Groundwater Resources Yield of Feixian County

  2. 提出了对于矿业开发过程中所扰动的地下水资源量和水质的保护方法,并进行了地下水环境监测方法研究,提出了完善的地下水环境保护方法体系。

    This paper proposed groundwater resources and water quality protection methods system .

  3. 黄河流域浅层地下水资源量及可开采量分析

    Analysis on Shallow Groundwater Resources and Exploitable Volume of the Yellow River Basin

  4. 河川基流分割法在山丘区地下水资源量评价中的运用

    Application of River Base Flow Separation in the Evaluation of Groundwater Resources in Mountainous Areas

  5. 地下水资源量受多项因素影响,是一动态随机过程。

    Groundwater resources may be influenced by multinomial factors , which is a dynamic random process .

  6. 西北诸河区各省(区)地下水资源量评价及其分布特征

    Evaluation of Groundwater Resources Quantity and Its Distribution Characteristics in Some Provinces ( Districts ) of the Northwest Catchment 's Area

  7. 计算了郑州市地表水资源量、地下水资源量、水资源总量和水资源可利用量。

    The quantity of surface water and ground water , water resources gross and its available quantity of these years are calculated .

  8. 二是提高了山丘区地下水资源量评价的精度,为探索山丘区地下水资源量及时空分布规律提供技术支撑。

    Thus , the research provides technique support for exploration of the groundwater resources and temporal and spatial rules in mountainous areas .

  9. 对洛阳市的降水量、地表水资源量、地下水资源量及水资源总量进行评价。

    The precipitation , surface water resources , groundwater resources , and total volume of water resources were evaluated for Luoyang City .

  10. 河水基流量是地下水资源量,应从地表水径流量中扣除。

    The base discharge of river is a type of amount of ground water resource which should be deducted from surface water discharge .

  11. 将难以利用的地下水量从地下水资源量中扣除后可得地下水实际可利用量。

    The available groundwater is equal to the total amount of groundwater subtracting the part of groundwater , which is hard to use .

  12. 采用总排泄法和有限元法对研究区地下水资源量进行了评价,并对未来6年地下水水位进行了预测。

    The paper used drainage method of ground water and finite element method assessed groundwater resources and forecasted the water table in the future six years .

  13. 分别用水均衡法和干扰井群法评价了地下水资源量,提出了地下水源开采井设计方案;

    The paper uses the theory of water balance and the disturbance well group to estimate the quantity of groundwater , and puts forward a project scheme for groundwater exploitation ;

  14. 重点探讨了区域地表水资源量、地下水资源量、水资源总量、区域可供水量的计算方法和区域水资源质量评价的方法;

    The methods to calculate the amount of regional surface water , ground water , the total amount of regional water resources and the amount of water resources which can be used are discussed ;

  15. 使狭义水资源的构成发生了变化,即地表水资源量减小、不重复量和地下水资源量增加。

    Soil and water conservation changes the composition of narrow sense water resources , that is amount of surface water resources decreased , amount of unrepeated water resources and water ground water resources increased .

  16. 然后对西宁市市的水资源进行了分析评价,包括降水量、地表及地下水资源量评价、水资源总量计算以及出入境水量分析计算。

    Analysis and evaluation of the water resources of the city of Xining City , including precipitation , surface and groundwater resources evaluation , calculation of total water resources as well as entry and exit of water analysis and calculation .

  17. 采用水均衡法评价黄河流域平原区多年平均浅层地下水资源量,采用可开采系数法评价全流域平原区多年平均浅层地下水可开采量。

    The paper evaluates the many years average shallow groundwater of plain area in the Yellow River basin by using water balance method and evaluates the many years average exploitable volume of shallow groundwater of the whole basin by using exploitable coefficients .

  18. 根据江西省第二次地下水资源量评价成果,探讨了山丘区地下水资源量的评价方法,供水资源管理、科研设计部门参考使用。

    Based on the second evaluation result of the groundwater quantity of Jiangxi province , several kinds of evaluation methods of ground water resources guantity massif regions was discussed . It can be referred for water resource management and scientific research and water design department .

  19. 但长期以来,地下水资源量评价使用费工费时费钱的大型抽水试验方法,其存在的问题有:一是长时间大量抽取地下水造成宝贵的地下水浪费;二是工作成本高、效率低。

    For a long time , groundwater resource evaluation by the use of labor intensive and time-consuming and costly large-scale pumping test method , its problems are : First , for a long time a large number of abstraction of groundwater wasted ; Second , working inefficient .

  20. 先解逆问题反演求参,再解正问题计算地下水开采资源量。

    Then the positive problem is solved to calculate groundwater resources .

  21. 体积法求解地下水的资源量

    Calculation for Groundwater Resources with Method of Volume

  22. 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 .

  23. 地下水资源的量与质就是该地区的城市节水办公室及水务局的水资源管理办公室工作的主要对象。

    The quantity and quality of groundwater are main working objects of local water-saving office as well as water resource management office of water-affair bureau .

  24. 特长隧道由于开挖工程量巨大、施工周期长,引起的山体地下水资源损失量大等特点,形成了对工程区地质环境状况的较大改变。

    Because of such characteristics as huge volume of excavation , long construction period , and significant loss of underground water resource , extra-long railway tunnel may greatly change geological environment situation of project area .

  25. 采用排泄法、均衡法等方法计算出各分系统内的地下水天然资源量、可采资源量,对地下水资源的分布特征进行了分析;

    Then the quantity of groundwater natural resources and exploitable resources in each sub-system was calculated by the methods of discharge method and water balance method , etc. The distribution properties of groundwater resources were analyzed .

  26. 因而需要保护水源、减少污染,提高地表水资源开发利用程度,进而限制和降低地下水资源开采量,可持续利用有限的水资源。

    Therefore need to improve the degree of development and utilization of water resources of the earth 's surface , and then restrain and reduce the exploiting amount of groundwater resources , limited water resource of sustainable utilization .

  27. 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 .

  28. 随着气候的变化、河道上游修建水库和工农业用水量的增加,地表水资源量逐年减少,地下水资源开采量逐年增加。

    Because of the transformation of the climate , the construction of the reservoir and the increasing consumption of water in industry and agriculture , the surface water resources are reduced year by year at the same time , the exploration of the ground water is increasing .

  29. 通过水均衡法计算1980-2000年全市地下水可采资源量为26.05亿m3。

    Computed according to the water balance method , city groundwater exploitable yield from 1980 to 2000 is 26.05 × 108 m3 .

  30. 柳林泉域岩溶地下水资源可开采量的确定

    Determination on Exploitable Quantity of Karst Ground Water in Liulin Spring-field