1) non-compression aquifer
无压含水层
2) infinite aquifer
无限含水层
3) confined aquifer
承压含水层
1.
Study on determination of parameters for confined aquifer with Whole Curve-Matching Method;
用全程曲线拟合法确定承压含水层参数的研究
2.
A mathematical water-pumping model of single wells withdrawing water from confined aquifers and its analytical analysis considering soil-particle movements;
考虑土体颗粒运动的承压含水层单井抽水数学模型及其解析分析
3.
Analysis of steady under-groundwater flow in the confined aquifer by finite layer method;
承压含水层地下水稳定流的有限层分析
4) high-pressure water-bearing stratum
高压含水层
1.
To avoid water bursting,this paper introduces the technology of grouting in high-pressure water-bearing stratum,which provides feasible experience for tunneling security.
主要介绍了对高压含水层的注浆堵水工艺,为巷道的安全掘进、防止巷道突水提供了可行的借鉴经验。
5) piezometric head
含水层水压力
6) semi-infinite aquifer
半无限含水层
1.
Well flow in semi-infinite aquifer is calculated with analytical method,the well flow near the linear recharge boundary is modeled with numerical method.
针对解析方法求解半无限含水层井流问题,对直线补给边界附近的井流采用数值方法进行模拟计算,并将两种方法进行比较,数值计算结果表明,存在补给边界时,抽水一定时间以后降深能达到稳定,但仅仅代表观测点处降深达到稳定,而整个渗流场并未达到稳定状态。
2.
In a semi-infinite aquifer bounded by a channel,a transient flow model is constructed for phreatic water subjected to vertical and horizontal seepage.
对河渠边界控制的半无限含水层,建立垂向入渗与河渠水平渗透共同作用下的潜水非稳定渗流模型;利用Boussinesq第一线性化方法,通过Laplace变换,给出模型的解析解。
补充资料：受压含水层
confining aquifer ，雨水降落地面后，一部份沿地面流至河海一部份渗透入土壤中。其中一小部份附着于土壤颗粒表面成为附着水，其余受重力作用渗入地下达到不透水层。此地下水受水力坡降的作用开始横向流动，土壤空隙充满水无空气存在，称含水层。如果含水层在两不透水层中间则称为受压含水层，其静水压力较大气压力为高。
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