000 01677nam a2200313Ia 4500
001 000008360
003 MX-MdCICY
005 20260113161404.0
008 981016s1998 nyua f p 001 0 eng d
020 _a044450155X (pbk.)
020 _a0444815465 (hardcover)
020 _a978044450155X (pbk.)
040 _cCICY
082 0 4 _a551.48
_bI86 1998
245 1 0 _aIsotope tracers in catchment hydrology /
_cedited by Carol Kendall, Jeffrey J. McDonnell
264 3 1 _aAmsterdam ; New York :
_bElsevier,
_c1998
300 _axxix, 839 p. :
_bil. ;
_c25 cm.
504 _aIncluye referencia bibliográfica: p. 804-816 e índice
520 3 _aIsotope tracers have been an important too. in catchment hydrology for the past two decades. Isotope hydrograph separations determined by simple conservative-mixing models have shown repeatedly that streamflow generated during rainfall or snowmelt is supplied largely by water stored in the catchment prior to the event. an insight that has greatly changed how hydrologists view how waters and solutes move from the land surface into streams and groundwater. Other uses of isotopes for tracing physical mixing and biogeochemical transformations have revolutionized our perception of catchments as integrated physical-chemical-biological systems
650 1 4 _aCUENCAS HIDROGRAFICAS
650 1 4 _aGEOLOGIA ISOTOPICA
650 1 4 _aGEOQUIMICA
650 1 4 _aQUIMICA AMBIENTAL
650 1 4 _aRADIOISOTOPOS EN HIDROLOGIA
700 1 2 _aKendall, Carol,
_eed.
700 1 2 _aMcDonnell, Jeffrey J.,
_eed.
856 4 0 _uhttps://www.cicy.mx/sitios/sib/doctoelectronico/8360.pdf
_zVer tabla de contenido y/o resumen
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_cBK
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