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| 基岩裂隙水水位沿程变化曲线方程的实验研究 | |
| 引用本文： | 钱家忠,李长青,李开红,刘咏.基岩裂隙水水位沿程变化曲线方程的实验研究[J].安徽地质,2001,11(2):158-160. |
| 作者姓名： | 钱家忠 李长青 李开红 刘咏 |
| 作者单位： | 1. 合肥工业大学资源与环境科学系,安徽,合肥,230009 2. 焦作矿务局,河南,焦作,454000 3. 焦作市市政工程公司,河南,焦作,454000 4. 合肥工业大学生物与食品工程系,安徽,合肥,230009 |
| 摘 要： | 本文根据室内模拟实验，研究了不同条件下隙宽小于3mm单一裂隙基岩水水位沿程变化曲线，验证了孙峰根等人建立的单一裂隙基岩水水位沿程变化的曲线方程。结论对基岩水运动理论的研究具有重要的参考价值。 |
| 关 键 词： | 单一流迳 基岩裂隙水 水位沿程变化方程 模拟实验 |
| 文章编号： | 1005-6157(2001)02-0158-03 |
| 修稿时间： | 2001年5月30日 |
EXPERIMENTAL STUDY ON BEDROCK WATER TABLE CHANGING WITH DISTANCE IN A SINGLE FRACTURE WITHIN 3MM WIDTH |
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| QIAN Jia zhong,LI Chang qing,LI Kai hong ,LIU Yong.EXPERIMENTAL STUDY ON BEDROCK WATER TABLE CHANGING WITH DISTANCE IN A SINGLE FRACTURE WITHIN 3MM WIDTH[J].Geology of Anhui,2001,11(2):158-160. | |
| Authors: | QIAN Jia zhong LI Chang qing LI Kai hong LIU Yong |
| Institution: | QIAN Jia zhong1,LI Chang qing2,LI Kai hong 3,LIU Yong4 |
| Abstract: | According to the data obtained from the simulation experiment,the curves of bedrock water level changing with distace in a single fracture within 3mm width under different conditions have been studied.The curve equations established in former study(by Sun Fenggen et al.)about relationship between the bedrock water table and the distance in a single fracture have been tested and verified.This conclusion is of important reference value in studying the theory of the bedrock water motion. |
| Keywords: | single fracture flow in fracture of bedrock water table changing with distance simulation test |
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