Titlebook: Aquifer Test Solutions; A Practitioner’s Gui Leonid N. Sindalovskiy Book 2017 Springer International Publishing Switzerland 2017 Pumping an

濃縮

Error, Ambiguity, and Creativityion of the hydraulic characteristics of aquifers subject to pumpage from wells. An important supplement to this is a function of the software, enabling analytical evaluation of aquifer characteristics based on monitoring data, where the source of perturbation is variations in the surface level of a water body.

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寒冷

Foreshadow

ICLE

chisel

Leaky Aquifershe pumping well penetrates only one (the main) aquifer. The head in the adjacent aquifer is either constant throughout the pumping-test period or varies over time due to pumping. The storage of the aquitards can be taken into account.

FLOUR

Pumping Test near a Streamlculating the drawdown depending on river geometry and hydrodynamic conditions: (1) the stream is a boundary of the flow (Sect.?.) and (2) the stream is a boundary that does not limit the cone depletion (Sect.?.). Steady-state solutions for pumping from a well under the stream are considered separat

不能平靜

Horizontal or Slanted Pumping Wellsts from horizontal and slanted wells in a confined aquifer (Sect.?.), an unconfined aquifer (Sect.?.), or a leaky aquifer (Sect.?.). All solutions are given for aquifers of infinite lateral extent with vertical anisotropy taken into account.

使服水土

placebo-effect

Slug Tests monitoring the water-level recovery in the same well until its original value is attained. Basic analytical relationships for slug tests are given for different experimental conditions. All such relationships take into account the wellbore storage.