Contributions in the field of soil chemistry have immensely benefited human
kind, including enhanced agricultural production and the quality of our env
ironment. This review focuses on research breakthroughs since the mid-1970s
and delineates frontiers in soil chemistry for the upcoming decade. Howeve
r, early contributions in ion exchange, sorption phenomena, and soil acidit
y are highlighted. Beginning in the 1970s, soil chemistry paradigms shifted
from the chemistry of plant nutrient reactions/processes in soils to studi
es on environmental soil chemistry. The latter included research on: acid r
ain effects on soils and waters; trace metal/metalloid, environmentally imp
ortant plant nutrient, radionuclide, and organic chemical reaction mechanis
ms and retention; speciation of soil contaminants using chemical extraction
and molecular scale analytical techniques; facilitated colloid transport o
f metals and organic chemicals; humic substance structure; kinetics of soil
chemical processes; redox transformations of contaminants in soils; modeli
ng of soil chemical reactions; and soil remediation. Frontiers in soil chem
istry over the next decade will undoubtedly involve the use of advanced in
situ technologies in combination with interdisciplinary research efforts to
unlock important information on: speciation of contaminants in soils; cycl
ing of trace elements and nutrients and impacts on global climate change; d
evelopment of models to accurately predict the rate, fate, and transport of
contaminants in the subsurface environment; elucidation of mechanisms for
microbial transformations of contaminants; unraveling the precise structure
of soil organic matter; and enhanced understanding of rhizosphere chemistr
y. In summary, the future of soil chemistry is bright for the 21st century.
(C) 2001 Elsevier Science B.V. All rights reserved.