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deep well
The KT2 strain of thermophilic spore-forming bacteria was isolated from a biofilm on the surface of a corroded pipeline in an extremely deep well (4680 m, 40-72°C) in the Urals.
      
A baryonic string has a Y-like shape with a deep well in the region of the string-junction position.
      
The generation of vortexlike structures in the case of stalled turbulent flow streaming around a deep well on a plane is analyzed.
      
Biomarker monitoring along the column of a deep well reflected the hydrodynamics determined both by geological conditions and exploitation of the well.
      
On the basis of the partial differential equations of the water level in a deep well that is affected by the bulk strain tide, the boundary conditions of permeating each other between aquifer and well are considered.
      
We have found precursory phenomena of water table in deep well before mining-induced earthquake.
      
Here we discuss the physical mechanism of coseismic effect of mining-induced earthquake on water table in deep well.
      
1) A set of period components corresponding well to those of Earth tides and barometric pressure can be separated from the hydro-spectra of deep well.
      
The basic frequency of the confined aquifer with a deep well for geo-acoustic observation, located at Juxian county, Shandong province, China, is 35.0 Hz.
      
Possible consequences are worked out in one dimension which includes relating supersymmetry to the infinite deep well problem
      
The global minimum occurs for the bent Li...FH structure at R=1.95?? and θ=70° with a relatively deep well of De=1,706?cm-1 and the secondary minimum is found for the linear Li...HF configuration at R=4.11?? with a well depth ofDe=288?cm-1.
      
The stable carbon isotopic ratio indicated that the HCO3- in the groundwater, excluding deep well water, originated from CO2 gas produced by organic matter in the soil.
      
The deep well water, which had a higher concentration of HCO3- than the other groundwater sampled, was thought to have acquired HCO3- though contact with rocks.
      
The36Cl/Cl ratio indicated the recharge age of the deep well water sampled at a depth of 760 m at the foot of the plateau was recent.
      
Unconfined aquifers of the proximal part of the fan delta contain 1~7?mg/l of DO, and a 250-m deep well still has an unusual value of 1.83?mg/l.
      
Using statistical and artificial neural network models to forecast potentiometric levels at a deep well in South Texas
      
Heat flow variation with depth in Poland: evidence from equilibrium temperature logs in 2.9-km-deep well Torun-1
      
High-precision temperature measurements were carried out up to a depth of 2,930?m in the 5.5-km-deep well Torun-1, 26?years after completion of drilling.
      
Comparison of hydrogeologic parameters evaluated by deep well testing programs to assess nuclear waste repository feasibility
      
Hydrogeologic parameters evaluated for rocks investigated in deep well testing projects for nuclear waste repository feasibility are transmissivity, hydraulic conductivity and storativity.
      
 

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