Results 221 to 230 of about 20,693 (272)
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Fate and distribution of 14C-atrazine in a tropical oxisol

Chemosphere, 2000
The herbicide atrazine is the most commonly detected pesticide in groundwater world-wide. A new microcosm test-system was used to determine the fate of 14C-atrazine in a Brazilian oxisol. 14C Ring-labelled atrazine was applied in a mixture with the commercial product Gesaprim 500 (Novartis) at a rate of 3 kg ha-1.
Reiner Schroll
exaly   +3 more sources

Evaluation of mercury phytoavailability in Oxisols

Environmental Science and Pollution Research, 2018
Mercury is a metal which is potentially toxic for the environment. Many factors control its retention in the soil, such as cation exchange capacity, pH, clay content, organic matter, and redox potential. It is important to know the phytotoxic effects of soil Hg to prevent environmental contamination and its entry into the food chain. Several analytical
Lima, Francielle Roberta Dias de   +9 more
openaire   +2 more sources

Oxisols and Ultisols

2015
Landscapes associated with Oxisols and Ultisols in Taiwan are stable and old, measured in hundred thousands of years, and the thickness can be up to 5 m. Plinthite may be present resulted from alternative wet and dry cycles by fluctuating water tables.
Zueng-Sang Chen   +2 more
openaire   +1 more source

Monovalent Ion Adsorption by an Oxisol

Soil Science Society of America Journal, 1987
Abstract An experimental method was developed to measure simultaneously the net proton surface charge density (σ H ) and surface excesses of metal ( n M ) and ligand ( n L
Laurent Charlet, Garrison Sposito
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Mössbauer analysis of Brazilian Oxisols

Hyperfine Interactions, 1986
Three sets of Brazilian Oxisols have been analysed by Mossbauer spectroscopy at 290, 80 and 4.2 K. In most cases two resolved magnetic hyperfine patterns associated with aluminous goethite and hematite are resolved; their ratio is related to soil colour. Samples from a 3 m soil profile show that both oxides become decreasingly aluminium substituted and/
J. D. Fabris   +3 more
openaire   +1 more source

Chapter 9 Oxisols

1983
Publisher Summary The taxon of Oxisols contains intensively weathered soils, most of which occur in tropical or subtropical regions. As a rule, they are found on old land surfaces or in sediments that are derived from them, although they may also form in rapidly weathering materials.
A. Van Wambeke   +3 more
openaire   +1 more source

Positive Permanent Charge in Oxisols

Soil Science Society of America Journal, 1982
Abstract The existences of a positive permanent charge can be inferred from charge characteristics of highly weathered tropical soils; it was found to be related to isomorphous substitution of Ti(IV) for Fe(III) in iron oxides. Comparable near‐constant values were found from anion adsorption at pH 7.0 to 9.0.
Tessens, E., Zauyah, Siti
openaire   +1 more source

Bivalent Ion Adsorption by an Oxisol

Soil Science Society of America Journal, 1989
Abstract Surface excesses of the bivalent ions Ca 2+ , Mg 2+ , and SO 2‐ 4 were measured on a Brazilian Oxisol suspended in Ca(ClO 4 )
Charlet, Laurent, Sposito, Garrison
openaire   +2 more sources

Phosphate Adsorption on an Oxisol

Soil Science Society of America Journal, 1977
Abstract Adsorption isotherms for phosphate on the A and B horizon of an oxisol from Papua New Guinea showed high affinity adsorption at low solution concentrations and a linear increase in adsorption at higher solution concentrations. Adsorption increased with decrease in pH in the range 3 to 8.
openaire   +1 more source

57Fe Mössbauer studies of oxisols

Hyperfine Interactions, 1991
Mossbauer spectroscopy is a valuable complement to the standard analytical techniques of soil science for characterizing the iron content of soils, and for studying the mineralogical transformations that occur during pedogenesis from the point of view of the iron.
J. M. D. Coey   +2 more
openaire   +1 more source

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