地下水
地下水
지하수
GROUNDWATER
2014年
4期
20-23
,共4页
高宗军%刘晓笛%王敏%田红%于晨
高宗軍%劉曉笛%王敏%田紅%于晨
고종군%류효적%왕민%전홍%우신
抽水井%饱水介质场%三维%地下水流%运动特征
抽水井%飽水介質場%三維%地下水流%運動特徵
추수정%포수개질장%삼유%지하수류%운동특정
Pumping well%water-saturated medium%3D%groundwater flow%motion features
利用设计建造的抽水试验装置,采取多项潜水及承压水的抽水试验,获得大量的抽水井周围饱水介质场三维动态观测数据。试验发现:无论是潜水还是承压水状态,抽水井附近观测井的水位变化,均具有距抽水井愈远愈高、愈近愈低的漏斗状分布,抽水井附件的地下水位降落漏斗是显著的;同时发现每个观测井不同高度上的观测点的水位,均呈现上高下低的特征,说明地下水具有由上到下的运动分量,地下水由周边的供水边界向抽水井聚集运移时,运动方向是下斜向的,潜水如此,承压水也如此。分析认为,这是水头压力与水体自身重力同时起作用的结果。由此推断,在抽水时,靠近承压水含水层顶板存在强势水流,且越靠近补给源,这种强势水流越强。
利用設計建造的抽水試驗裝置,採取多項潛水及承壓水的抽水試驗,穫得大量的抽水井週圍飽水介質場三維動態觀測數據。試驗髮現:無論是潛水還是承壓水狀態,抽水井附近觀測井的水位變化,均具有距抽水井愈遠愈高、愈近愈低的漏鬥狀分佈,抽水井附件的地下水位降落漏鬥是顯著的;同時髮現每箇觀測井不同高度上的觀測點的水位,均呈現上高下低的特徵,說明地下水具有由上到下的運動分量,地下水由週邊的供水邊界嚮抽水井聚集運移時,運動方嚮是下斜嚮的,潛水如此,承壓水也如此。分析認為,這是水頭壓力與水體自身重力同時起作用的結果。由此推斷,在抽水時,靠近承壓水含水層頂闆存在彊勢水流,且越靠近補給源,這種彊勢水流越彊。
이용설계건조적추수시험장치,채취다항잠수급승압수적추수시험,획득대량적추수정주위포수개질장삼유동태관측수거。시험발현:무론시잠수환시승압수상태,추수정부근관측정적수위변화,균구유거추수정유원유고、유근유저적루두상분포,추수정부건적지하수위강락루두시현저적;동시발현매개관측정불동고도상적관측점적수위,균정현상고하저적특정,설명지하수구유유상도하적운동분량,지하수유주변적공수변계향추수정취집운이시,운동방향시하사향적,잠수여차,승압수야여차。분석인위,저시수두압력여수체자신중력동시기작용적결과。유차추단,재추수시,고근승압수함수층정판존재강세수류,차월고근보급원,저충강세수류월강。
By using pumping test device designed and made by the author, the author gets a groups of 3 D observation data on water level variations of water-saturated medium around pumping wells. The research shows that for both phreatic water and confined water, the water level of observation well falls when it closes to the pumping well. The water level variation curve presents itself as a funnel with the location of the pumping well as the core. At the same time, the water heads of different ob-servation points at different heights of each observation well are higher to lower from top to bottom, which is characterized by showing that the water has a top to bottom motion component while groundwater has migration and accumulation from the sur-rounding water boundary to the pumping well, i. e. the water movement direction is inclined. The same is true for artesian wa-ter. It is a result of the combined action of water head pressure and the gravity of groundwater itself. Accordingly, the paper makes the conclusion that there is powerful groundwater flow near the artesian aquifer. The groundwater flow becomes more powerful when it close to the recharge source.