Relative mobility of the common elements in weathering of some schist and granite areas

Autor:	H.E Hawkes, D.H Anderson
Rok vydání:	1958
Předmět:	geography Mineral geography.geographical_feature_category Geochemistry and Petrology Homogeneous Schist Geochemistry Drainage basin Mineralogy Composition (visual arts) Weathering Geology
Zdroj:	Geochimica et Cosmochimica Acta. 14:204-210
ISSN:	0016-7037
DOI:	10.1016/0016-7037(58)90079-6
Popis:	Chemical analyses were made of stream waters and rocks from three local drainage basins within, which the rocka are chemically homogeneous. The relative mobility of each major element was computed as the ratio of its content in the mineral residue of the stream water to its content in the rock drained by the stream. The order of mobility in each case was Mg > Ca > Na > K > Si > Al = Fe. This differs somewhat from published estimates based on the composition of average fresh waters and rocks, in which the reported order of mobility was Ca > Na > Mg > K > Si > Al = Fe.
Databáze:	OpenAIRE
Externí odkaz:	https://explore.openaire.eu/search/publication?articleId=doi_________::dc1f20cd63908acaf4c24730790d5052 https://doi.org/10.1016/0016-7037(58)90079-6 Zobrazit plný text záznamu