D. C. Bain

Rochester Institute of Technology

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M. J. Wilson

University College London

D. M. L. Duthie

Cairn Research (United Kingdom)

Stephen Guggenheim

University of Illinois Chicago

Emilio Galán Huertos

Universidad de Sevilla

M. L. L. Formoso

Universidade Federal do Rio Grande do Sul

Maria Franca Brigatti

University of Modena and Reggio Emilia

W. J. McHardy

Institut National de la Recherche Agronomique

V. A. Drits

Geological Institute

Helge Stanjek

RWTH Aachen University

Simon Langan

International Water Management Institute

Cooperative Institutions

Chalfonts and Gerrards Cross Hospital

Senologic Hellenic Society

Oxford University Press (United Kingdom)

Louisiana State University

Macaulay Development Trust

Swedish University of Agricultural Sciences

University of Aberdeen

Centre National de la Recherche Scientifique

University College London

James Hutton Institute

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Chemical and mineralogical forms of lead, zinc and cadmium in particle size fractions of some wastes, sediments and soils in Korea

Applied Geochemistry (1999)

Young Duk Song M. J. Wilson Hong‐Seok Moon Jeffrey R. Bacon D. C. Bain

Fraction (chemistry)

10.1016/s0883-2927(98)00093-6

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Citations (56)

Spheniscidite, a new phosphate mineral from Elephant Island, British Antarctic Territory

Mineralogical Magazine (1986)

M. J. Wilson D. C. Bain

Abstract Spheniscidite is a new phosphate mineral occurring in a soil profile in an area of nesting penguins on Elephant Island. It is the NH 4 -dominant analogue of leucophosphite and has the formula (NH 4 ,K)(Fe 3+ ,Al) 2 (PO 4 ) 2 (OH) · 2H 2 O. It is monoclinic, P2 1 /n with unit cell parameters a = 9.75, b = 9.63, c = 9.70 Å, β = 102° 34′, and Z = 4. The strongest X-ray lines are 6.79(100), 5.99(90), 3.05(45), 7.62(40) Å. Spheniscidite is thought to have formed by the interaction of ammonium phosphate solutions from penguin guano with micaceous and chloritic minerals in the soil. The name is for Sphenisciformes, the order name for penguins, and has been approved by the IMA Commission on New Minerals and Mineral Names.

Guano

Monoclinic crystal system

10.1180/minmag.1986.050.356.14

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Citations (22)

A preliminary review of weathering rates in relation to their method of calculation for acid sensitive soil parent materials

Water Air & Soil Pollution (1995)

Simon Langan Mark E. Hodson D. C. Bain R. A. Skeffington M. J. Wilson

Base (topology)

10.1007/bf00477124

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Citations (25)

A sodium hydroxide fusion method for the determination of total phosphate in soils

Communications in Soil Science and Plant Analysis (1982)

B. F. L. Smith D. C. Bain

Abstract Total phosphate in soils can be determined at low cost using a sodium hydroxide decomposition technique followed by spectro‐photometric measurement in solution. The fusion, in nickel crucibles, is more rapid and takes place at a much lower temperature than the conventional fusion with sodium carbonate. Analyses compare well with published results for standard rocks and with analyses for a range of Scottish soils obtained by X‐ray fluorescence spectroscopy and by sodium carbonate fusion.

Sodium carbonate

Sodium hydroxide

10.1080/00103628209367257

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Citations (123)

Water Air and Soil Pollution Focus (2003)

Ulla S. Lundström D. C. Bain Andy F. S. Taylor Patrick A.W. van Hees

Soil acidification

Cation-exchange capacity

10.1023/a:1024115111377

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Citations (91)

An Unusually Interlayered Clay Mineral from the Eluvial Horizon of a Humus-Iron Podzol

Clay Minerals (1994)

D. C. Bain A. R. Fraser

Abstract The <2 µm fraction from the eluvial horizon of a humus-iron podzol is composed predominantly of a dioctahedral mineral with a basal spacing of 14.7 Å which contracts to 13.7 Å on solvation with glycol, and to 11.4 Å on heating to 300°C. The interlayer region is partially filled with an amorphous organo-Fe-Al complex which is very unstable and is affected by every treatment employed, even homoionic cation saturation. The mineral has a mica-like morphology, contains 3.4% non-exchangeable K 2 O and is considered to be an interstratified mica-vermiculite formed by the weathering of mica. The contraction of the basal spacing with glycol is probably due to water being removed from the interlayer region of the vermiculite component, leaving only the natural organo-complex in the interlayer; alternatively, the contraction may be more apparent than real, resulting from an interstratification effect. Treatment with H 2 O 2 results in partial expansion with glycol.

Eluvium

Vermiculite

Humus

Podzol

10.1180/claymin.1994.029.1.08

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Citations (28)

Summary of recommendations of nomenclature committees relevant to clay mineralogy: Report of the association (vol 46, pg 586, 2006)

Clays and Clay Minerals (2007)

Stephen Guggenheim Jerry M. Adams D. C. Bain F. Bergaya Maria Franca Brigatti

Association (psychology)

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