最近30从www.hoelymoley.com 2023 - 07 - 10 - t21:28:01z //www.hoelymoley.com/feeds/question/13935 https://creativecommons.org/licenses/by-sa/4.0/rdf //www.hoelymoley.com/q/13935 1 "杰拉德贾马尔 //www.hoelymoley.com/users/12718 2018 - 04 - 19 - t10:07:24z 2018 - 04 - 19 - t13:28:54z

< p > < a href = " https://i.stack.imgur.com/aVmc5.png " rel = " nofollow noreferrer " > < img src = " https://i.stack.imgur.com/aVmc5.png " alt = "承压含水层的问题" > < / > < / p > < p >我不懂如何导致承压含水层的水自喷井达到一个水平高于地面?和水压面扮演什么角色? < / p >

//www.hoelymoley.com/questions/13935/-/13936 # 13936 6 potatasbravas //www.hoelymoley.com/users/12701 2018 - 04 - 19 - t13:28:54z 2018 - 04 - 19 - t13:28:54z

< p >红线或水压线的水平水想崛起——如果它被允许达到流体静力学平衡。自流条件地方下面埋藏着一个承压含水层水头水平(水平的水要上升)。在这种情况下,水是有限,不能达到水位,即使它想——这意味着它不是在流体静力学平衡。这个含水层被描述为有围压和静压头。如果你把一个在任何地方沿着这承压含水层,含水层的水会上升到红线的水平。< / p > < p >我想在你的案子的有点让人摸不着头脑,坐在上面的水压线整个承压含水层表明整个地区承压,但“流动”的条件只在水压线上方的实际表面,水会超越表面意义。另一个例子是,如果你是打井,向左或向右的突出显示区域,水将提高到这一水平,但仍将低于表面条件不会被描述为“流动”。< / p > < p > < a href = " https://i.stack.imgur.com/HQHrA.png " rel = " noreferrer " > < img src = " https://i.stack.imgur.com/HQHrA.png " alt = "在这里输入图像描述" > < / > < / p > < p > (< a href = " http://www.env.gov.bc.ca/wsd/plan_protect_sustain/groundwater/flowing_artesian_wells.pdf " rel = " noreferrer " > http://www.env.gov.bc.ca/wsd/plan_protect_sustain/groundwater/flowing_artesian_wells.pdf < / >) < / p >

map