نتایج جستجو برای: permeable layers because of clay and marl layers confined aquifer

تعداد نتایج: 24070389  

Journal: :caspian journal of enviromental sciences 0

water is the main option of any development, so having an accurate management of groundwater is necessary. this study has been done in damghan sedimentary plain in iran, which is located in northwest of semnan province. the main objective of this research was to estimate the rate and right site of recharge in damghan plain to prevent the aquifer from decreasing the water table. for this purpose...

2011
Aude Picard Timothy G. Ferdelman

Microbial heterotrophic activity was investigated in oxic sub-seafloor sediments at North Pond, a sediment pond situated at 23°N on the western flank of the Mid-Atlantic Ridge. The North Pond sediments underlie the oligotrophic North Atlantic Gyre at 4580-m water depth and cover a 7-8 million-year-old basaltic crust aquifer through which seawater flows. Discrete samples for experimentation were...

Journal: :Physical chemistry chemical physics : PCCP 2010
Luminita M Toma Régis Y N Gengler Eric B Prinsen Dimitrios Gournis Petra Rudolf

The Langmuir-Schaefer (LS) method has been investigated as a means to control the structure of hybrid organoclay thin films consisting of montmorillonite and dimethyldioctadecylammonium (DODA) cations. We observed a significant modification of the compression isotherms as a function of clay mineral concentration in the subphase, implying clay interaction with the alkylammonium monolayer. For a ...

A. Malekian B. Motamedvaziri Gh. Ashtiani M. Mahdavi

Water is the main option of any development, so having an accurate management of groundwater is necessary. This study has been done in Damghan sedimentary plain in Iran, which is located in northwest of Semnan Province. The main objective of this research was to estimate the rate and right site of recharge in Damghan plain to prevent the aquifer from decreasing the water table. For this purpose...

K. Belhassan

The Mikkes basin is located at the north center of Morocco. It comprises three different zones which represent diversified geologies which shelter a phreatic and confined aquifer in the Sais basin and a shallow aquifer in the Tabular Middle Atlas. The springs in the Sais phreatic aquifer have suffered a maximum depletion. The springs with a deep or mixed origin are known as low flow variation s...

Journal: :Dutse Journal of Pure and Applied Sciences 2023

In this study we estimated the aquifer hydraulic parameters of Damaturu, Yobe State, Nigeria, using electrical resistivity method. Schlumberger configuration was adopted for study. Five geologic layers, which are Topsoil, Clay, Sand, Sandy-clay, and Sand were delineated in area. The results measured revealed that values area ranged from 126 to 518 Ωm has an average 328 Ωm. thickness 39 71m with...

2007
Peter A. Stone

The distribution of ground-water radiocarbon ages from the Tertiary limestone aquifer (includes the Floridan aquifer) in South Carolina shows both a typical trend for a regional sedimentary aquifer plus a lesscommonly reported occurrence of disjunct outliers of recharging and thus high vulnerability to contamination located farther down the regional flow system. The main recharge area, and thus...

Journal: :Land 2023

In this paper, we use interferometric synthetic aperture radar (InSAR) annual and time-series analysis of RADARSAT-2 SAR data, spanning from September 2011 to October 2022, study the temporal–spatial characteristics land subsidence in Hengshui, North China Plain. The data reveal two large-scale areas individually located north Hengshui city around Hutuo River east or south along Fuyang, Suolu Q...

Journal: :iranian journal of earth science 0
k. belhassan ufr: geology applied to hydro-geological researches. faculty of sciences dhar mehraz b.p. 1796 fez atlas. 30 003. fez. morocco.

the mikkes basin is located at the north center of morocco. it comprises three different zones which represent diversified geologies which shelter a phreatic and confined aquifer in the sais basin and a shallow aquifer in the tabular middle atlas. the springs in the sais phreatic aquifer have suffered a maximum depletion. the springs with a deep or mixed origin are known as low flow variation s...

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