1) water-rich belt
富水带
1.
The exploratory result shows that two water-rich belts tend- ing towords to NE in the fourteenth limestone aquifer in the seam floor and a irregular-shaped water-rich belt li.
探查结果表明,工作面底板十四灰含水层存在近 SN(西部)和 NE 向(东部)两个富水带;奥灰含水层在工作面中东部存在一条不规则状富水带。
2) water abundant area
富水区带
1.
By the method of karst in borehole and time domain electromagnetism analysis,the water abundant feature in Ordovician limestone was studied,water abundant area in mine was divided,hydro-geological information was full used,and the systemical method of water abundant area division was formed.
奥陶系灰岩富水区带划分是矿井水灾害预测与防治的基础,本文利用钻孔岩溶分析和瞬变电磁勘探相结合的水文地质研究方法,研究了奥陶系灰岩垂向上和平面上的富水性,划分了井田富水区带,实现了对矿井范围内水文地质信息的最大利用,形成了适合奥陶系灰岩富水区带划分的配套方法。
3) high pressure and enriched water region
高压富水带
4) water rich fractured band
富水断裂带
6) broken stone band aquifer
破碎带富水层
补充资料：经水带黄混浊
经水带黄混浊
病名。见清·沈尧封《女科辑要·卷上》。指月经色黄夹杂混浊液体者。多由脾虚失运，湿痰下注所致。《女科辑要》引李氏：“经水带黄混浊者，湿痰也。”治宜健脾益气，除湿化痰。方选二陈汤加减。
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