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- MODELLING OF GEOCHEMICAL BEHAVIOR OF NEPTUNIUM, PLUTONIUM AND STRONTIUM IN A LOESS AQUIFER 镎、钚、锶在黄土地下水中地球化学行为的模拟研究
- loess aquifer 黄土含水层
- Most loess is considered to be an eolian deposit. 大多数黄土被认为是一种风成沉积。
- "The ancient, desolate loess plateau. “苍凉古老的黄土高原。
- Derive the governing flow equation for an aquifer. 推导地下含水层的流体方程式.
- Calculate aquifer properties based on well tests. 利用水井试验数据计算含水层的导水性质.
- 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。
- Huaxia Culture takes root in the loess plateau. 华夏文化深深地扎根于黄土高原。
- Loess, he had thought despairingly. 黄土，他绝望地想。
- Loess gulch nearing Hui Ning hsien. Feb. 13. 2月13日，会宁县附近的黄土峡谷。
- Township iscan yuan gully region of Loess Plateau. 全乡属黄土高原残垣沟壑区。
- Sometime the term artesian is used to denote a confined aquifer. 有时候人们也用自流含水层这一术语表示承压含水层。
- "The ancient, desolate loess plateau . “苍凉古老的黄土高原。
- A cloud of loess filled the whole sky. 黄土漫天。
- Mainly chernozem soil, followed by loess. 土壤主要是黑钙土，其次是黄土。
- Liang result for the northern Loess gully region. 北部为黄土梁峁沟壑区。
- A confined aquifer is also known as a pressure aquifer. 承压含水层又叫压力含水层。
- Such material can confine water in an artesian aquifer. 这样的介质能把水控制在承压含水层中。
- One of the two main types of aquifer is the unconfined aquifer. 非承压含水层是两种主要含水层之一。
- The aquifer is unconfined locally and may be recharged. 含水层因为局部不承压而得到补给。
