含水层的例句大全

Haven't been dug into the water-bearing stratum, the well certainly will not produce water.

这口井没打到含水层, 当然不会出水.

Aquifer storage ( ATES ) has become a relatively well-known storage technology in many parts of the world.

地下含水层储能已成为一项在世界上较为 知名 的储能技术.

The location and extent of aquifers is dependent upon the geological conditions of the underlying rock.

含水层的位置和范围是根据下垫岩石的地质条件所决定的.

So the risk of inadvertently contaminating the deep aquifers must be carefully weighed.

所以,深层含水层意外受污染的风险一定要小心考虑.

Recharge areas are necessary for a healthy aquifer.

补给区对于一个正常的含水层来说是必需的.

There is no experience on the gas-drive mechanism study of aquifer underground gas storages in China.

含水层储气库建库注气与驱动机理数值模拟设计和模拟思路都有其特殊性和复杂性,目前国内对此研究很少.

The spacial structure character of the fourth epoch aquiferous thickness in Tongliao area

通辽地区第四系含水层厚度的空间结构特征

Thirdly, to carry out experiments and studies on UGS in oil reservoir and aquifer;

在油藏和含水层储气库领域进行实验和摸索；

For PRW, the seasonal thermal energy storage ( STES) alleviated the dependency on aquifer for heat source or sink, and made aquifer as a carrier for heat storage.

抽灌同井运行时的季节性储能很大程度地减轻了对含水层作为热源（汇）的依赖，而让其作为一种蓄热的载体。

Experimental Study on Removal of Adsorbable Organic Halogen ( AOX) by Soil Aquifer Treatment

土壤含水层处理去除可吸附有机卤化物的试验研究

The rock in the fault zones in mine roadways are generally fractured and difficult to support.

矿山巷道中的断层带岩石一般比较破碎,难以支护,而且常常与含水层导通,易发生涌水.

Research on the Mining on the Coal Face without Sand Control Seam under the Poor Water-Content Loose Aquiclude

双层含水层系统的数值计算方法弱松散含水层下无防砂保护层开采研究

In addition , we found a obvious groundwater divide on the south side of Ma-An river.

中层是为封闭的含水层, 深层地下水在枯水季有高山区域流达的水源.

The Archaean era limestone aquifer close to No. 10 coalbed is the direct aquifer of it.

距离其较近的太灰含水层，是10煤开采的直接充水含水层。

Water source includes aquiferous layer, river, water-eroded cave, goaf seeper, preferred faults with abundant groundwater.

水源包括含水层、江河、溶洞和采空区积水、洪水倒灌水、富水优势断裂；

An aquifer is a layer of underground rock or sand which stores and carries water.

含水层是保存和携带着水的一层地下的水或沙.

In Chengde area, water table is shallow, gravel bed is the main aquiferous layer and its penetrability coefficient is comparatively large, settlement radius caused by dewatering is large as well.

承德地区地下水位较浅，含水层主要为圆砾层，并且渗透系数较大，基坑降水引起的地面沉降半径也较大。

By analyzing the physical geography, regional hydrology and geology information, and groundwater equilibrium of DunHuang Basin, this paper simulates the aquiferous layer which has the thickness of 250 m, and consider it as two dimension mixed layer which is heterosphere and isotropy.

通过敦煌盆地自然地理和区域水文地质及盆地地下水均衡分析，将250m左右深度处稳定流线以上的含水层作为数值模拟对象，概化为非均质各向同性平面二维流混合层；

Both the shallow and deep aquifers are highly over-exploited a large area of Hai river basin.

海河平原的的浅层和深层含水层大面积处于严重超采状态.

Two methods, i.e.integrated factor method and correlativity method for recognizinghydrochemical features of basal water and water gush source are introduced in this paper.

本文论述了识别主要含水层水化学特征和突水水源的二种方法，即综合要素法和灰色关联度法。