关于承压水井周“紊流”的问题,多年来有不少的学者进行过研究。多数人认为,井周所以出现地下水流速(V)与水力坡度(I)的曲线关系,是紊流引起的。也有少数人认为,井周出现的这种非线性渗流,不一定都是紊流引起的。因为1955年法国人施内贝利在巴黎Dhatou水力实验室用染色法对玻璃球和砾石作过试验,他发现水还处在 Regarding the problem of “turbulent flow” in confined wells, many scholars have conducted research over the years. Most people believe that the relationship between groundwater velocity (V) and hydraulic gradient (I) is the result of turbulence. There are also a few people who believe that this kind of non-linear seepage occurring around the well is not always caused by turbulence. Because in 1955 the Frenchman Schnebelli tested the glass balls and gravel with dyeing at the Dhatou Hydraulic Laboratory in Paris, he found that the water was still in