Zobrazeno 1 - 7
of 7
pro vyhledávání: '"W. Michael Edmunds"'
Autor:
Jinzhu Ma, W. Michael Edmunds
Publikováno v:
Hydrogeology Journal. 14:1231-1243
The amount and timing of aquifer recharge and the evolution of lakes and groundwater in the south-eastern Badain Jaran desert of Inner Mongolia, with high megadunes, has been investigated using stable isotopes and hydrochemistry. Unsaturated zone moi
Autor:
W. Michael Edmunds, K. E. Keese, Ian Simmers, Bridget R. Scanlon, C.B. Gaye, Alan L. Flint, Lorraine E. Flint
Publikováno v:
Hydrological Processes. 20:3335-3370
Global synthesis of the findings from ∼140 recharge study areas in semiarid and arid regions provides important information on recharge rates, controls, and processes, which are critical for sustainable water development. Water resource evaluation,
Three-dimensional flow and trace metal mobility in shallow Chalk groundwater, Dorset, United Kingdom
Publikováno v:
Journal of Hydrology. 292:229-248
The three-dimensional groundwater flow and the hydrogeochemical regime have been determined in the Bere Stream valley, North Dorset Downs, southern England. The dual porosity characteristics of the Portsdown Chalk have been established using geophysi
Autor:
Zoran Radovanovic, W. Michael Edmunds
Publikováno v:
Environmental geochemistry and health. 13(2)
Until now failure has been a common feature of all attempts to elucidate the aetiology of Balkan endemic nephropathy (BEN), a peculiar kidney disease known to exist only in south-eastern Europe. However, whatever the cause, many epidemiological data
Publikováno v:
Zeitschrift der Deutschen Geologischen Gesellschaft. 145:143-152
Publikováno v:
Water Resources Research. 27:199-214
Stable isotopes, major elements, trace elements, and noble gases in groundwater from northern Mali permit a reconstruction of the paleohydrology of the Sahelian and sub-Saharan regions of west Africa. Major floods of the Niger River during the more h
Publikováno v:
Quarterly Journal of Engineering Geology. 9:73-101
Summary This paper presents a reconnaissance of naturally occurring trace element levels in the Triassic sandstones of the Wolverhampton area, and compares these with levels resulting from contamination. The three dimensional water quality variation