Ground water in the alluvial deposits of the Washita River between Clinton and Anadarko, Oklahoma

1963 ◽  
Author(s):  
D.L. Hart
1946 ◽  
Vol S5-XVI (4-6) ◽  
pp. 363-369
Author(s):  
Gaston Astre

Abstract Discusses the role of calcareous tufa deposits in the ground-water hydrology of dry valleys, citing two examples of the occurrence of calcareous tufa in alluvial deposits of dry valleys of the Quercy region, France. The tufa is considered the product of subterranean deposition from waters, which at one time had emerged as a spring and deposited tufa on the surface at the foot of the valley slope, but which later percolated along newly formed lower-level fissures.


1956 ◽  
Vol S6-VI (4-5) ◽  
pp. 531-546
Author(s):  
Louis Glangeaud ◽  
Solange Francois ◽  
Marie Jeanne Perrenoud ◽  
Robert Pezard ◽  
Michel Toitot

Abstract Discusses the exploration and exploitation of ground-water zones in the northern Jura region, France. Phreatic waters occur in Tertiary and Quaternary beds, and artesian aquifers in Mesozoic formations. The source, circulation, and recovery of waters in the karst and overlying alluvial deposits are treated in some detail.


1991 ◽  
Vol 24 (11) ◽  
pp. 111-116 ◽  
Author(s):  
Budimir Filipovic ◽  
Slobodan Vujasinovic ◽  
Ivan Matic

Drastic pollution case studies of entire complexes of alluvial deposits and water contained in them from polluted rivers have been recorded in more than one stream: beginning with the Sitnica to the Ibar, the Zapadna Morava and the Velika Morava to the Danube. A high phenol concentration (about 110 µg/l) in the Zapadna Morava in December 1983 affected the ground water reservoir - the source of Kruševac municipal water supply. Analysed samples indicated that phenol was transported by the Ibar River and its upstream tributary Sitnica from a coal gasification plant of a mine. Phenol concentrations were 364 µg in the Ibar at Kraljevo, 540 µg/l slightly more upstream, and up to 4000 µ.g/l upstream in the Sitnica near the source of pollution. Phenol concentrations in riparian ground water were even higher than in the rivers in some intervals. Nearly all sources were affected in the riparian zone downstream to the Danube. Occurrences of this pollutant in the ground water resources and certain experiences are considered in this paper.


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