The mobilization of aluminum in a natural soil system

effects of hydrologic pathways

I. M. Cozzarelli, J. S. Herman, Roderic A Parnell

Research output: Contribution to journalArticle

48 Citations (Scopus)

Abstract

A two-component soil water flow model was used in conjunction with an equilibrium speciation model WATEQF to study aluminum mobility in soils of a forested watershed, White Oak Run, in the Shenandoah National Park, Virginia. The deep soil is a sink for aluminum. Mineral solubility controls water chemistry in the deep soil, while organic substances are the key control in the shallow macropore waters. -from Authors

Original languageEnglish (US)
Pages (from-to)859-874
Number of pages16
JournalWater Resources Research
Volume23
Issue number5
StatePublished - 1987
Externally publishedYes

Fingerprint

Aluminum
aluminum
mobilization
Soils
Water
soil
Quercus alba
forested watersheds
macropores
macropore
hydrochemistry
water chemistry
water flow
solubility
national parks
national park
Watersheds
soil water
organic matter
watershed

ASJC Scopus subject areas

  • Aquatic Science
  • Environmental Science(all)
  • Environmental Chemistry
  • Water Science and Technology

Cite this

The mobilization of aluminum in a natural soil system : effects of hydrologic pathways. / Cozzarelli, I. M.; Herman, J. S.; Parnell, Roderic A.

In: Water Resources Research, Vol. 23, No. 5, 1987, p. 859-874.

Research output: Contribution to journalArticle

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