Basic BiogeographyFirst published in 1985. Routledge is an imprint of Taylor & Francis, an informa company. |
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Page 48
Optimum soil water conditions for most plants will occur between these two points
when the soil reaches field capacity. This is defined as when the amount of water
retained, just after the excess has drained away by gravity, is at its peak.
Optimum soil water conditions for most plants will occur between these two points
when the soil reaches field capacity. This is defined as when the amount of water
retained, just after the excess has drained away by gravity, is at its peak.
Page 59
5, Soil Survey of England and Wales, Harpenden. Huggett, R. J., 1982. 'Models
and spatial patterns of soils', In Principles and Applications of Soil Geography (
eds Bridges, E. M. and Davidson, D. A.), Longman, London and New York, pp.
5, Soil Survey of England and Wales, Harpenden. Huggett, R. J., 1982. 'Models
and spatial patterns of soils', In Principles and Applications of Soil Geography (
eds Bridges, E. M. and Davidson, D. A.), Longman, London and New York, pp.
Page 285
SOIL SURVEY AND MAPPING The most comprehensive accounts of British soils
are contained in the Regional Memoirs produced by the Soil Survey of England
and Wales. They describe soils and their properties from the viewpoint of the ...
SOIL SURVEY AND MAPPING The most comprehensive accounts of British soils
are contained in the Regional Memoirs produced by the Soil Survey of England
and Wales. They describe soils and their properties from the viewpoint of the ...
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Contents
Introduction | 3 |
Initial approaches to vegetation study | 12 |
Initial approaches to soil study | 34 |
Copyright | |
9 other sections not shown
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acid activities agricultural animals approach areas associated become Britain British brown cause cent changes chemical Class clay climatic complex conservation cover crop cycle detailed determined disturbance dominant early ecology ecosystem effects energy environment environmental established example exist factors field fire flora forest further grass grazing ground growing growth horizon humus important increase influence insect land layer lead less limit litter loss major material measure methods mountain natural North nutrients oakwood occur organic particularly pattern peat period pest pine plant population present problem processes production reached recent reference region relatively shown similar slopes soil species spread stage stands structure succession surface Table temperature trees types unit upland usually values vegetation wind wood woodland zone