1) two-aquifer systems
双含水层系统
2) aquifer system
含水层系统
1.
Lithofacies-based study of the structure of the aquifer system of the Cretaceous Ordos basin, China;
基于岩相的鄂尔多斯白垩系盆地含水层系统结构的研究
2.
Relation between water level and water temperature in the aquifer system of Changli well and seismicity;
昌黎井含水层系统的水位水温动态关系与地震活动
3.
According to the hydrology geology condition,this paper discusses the principle of the division that is the absolute aquifer system and integrated water circulation.
本文根据四平市水文地质条件,探讨了四平市地下水系统划分的原则,即拥有独立的含水层系统和完整的水循环系统。
3) confined aquifer system
承压含水层系统
1.
Stress-strain characteristics of the confined aquifer system and land subsidence controlling countermeasures in Shanghai;
上海市承压含水层系统应力-应变特征及地面沉降防治对策
2.
Generally, according to the idea of responding matrix method among groundwater resource management models, a two-dimension (2D) confined aquifer system can be divided into two subsystem which are the one formed by artificial activities and the one formed under natural supplying/draining conditions.
根据地下水资源管理模型响应矩阵法的建模思想,一般的二维承压含水层系统可分解为两个承压含水层子系统,一个为由人工干扰作用下的,另一个为由天然补径排条件作用下的。
4) porous aquiferous stratum system
孔隙含水层系统
1.
By analyzing the problem of hydrological 3D spatial dispersion in 3D finite differential numeric simulation of porous groundwater flow, as well as discontinuous spatial distribution and asymmetric thickness of porous aquiferous strata and partitive groundwater stratum, the paper presents the GIS-based technique of 3D spatial dispersion of porous aquiferous stratum system.
分析了目前孔隙地下水流三维有限差分数值模拟中对含水层系统三维空间离散存在的问题 ,针对自然界孔隙含水层与隔水层空间分布的不连续性与厚度的不均匀性 ,研究了基于GIS的孔隙含水层系统三维空间离散实现的技术路线 ,提出了基于GIS与不规则六面体元的孔隙含水层系统的三维空间离散方法 ,最大限度地保证了离散体元中含水层类型的单一性 ,提高了孔隙地下水流模拟模型三维空间离散的精度 。
5) river-aquifer system
河流-含水层系统
1.
Variation process of hydrologic elements of river-aquifer system;
河流-含水层系统中水文要素的变化过程分析
6) unconfined aquifer parameter
含水层系统参数
1.
Boulton-RAGA method for identifying unconfined aquifer parameters;
确定潜水含水层系统参数的Boulton-RAGA方法
补充资料：含水层
见地下水。
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