The nature of three ancient woodland soils in southern England

Despite a wealth of published research on the nature of woodland soils, little is known about the nature of soils on sites that have supported woodland for many hundreds of years, namely ancient woodland. The properties and variability of soils in three ancient woods; one in the New Forest, Hampshir...

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Veröffentlicht in:Journal of biogeography 1997-09, Vol.24 (5), p.633-646
Hauptverfasser: Wilson, B. R., Moffat, A. J., Nortcliff, S.
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Nortcliff, S.
description Despite a wealth of published research on the nature of woodland soils, little is known about the nature of soils on sites that have supported woodland for many hundreds of years, namely ancient woodland. The properties and variability of soils in three ancient woods; one in the New Forest, Hampshire and two in Berkshire, were compared with those under recent woods. The acidity of ancient and recent woodland soils was high and remarkably similar. Only where cultivation of soils had preceded woodland establishment was soil acidity lower. The quantity of carbon in the soils studied was inversely related to soil acidity and the ancient woods had accumulated larger quantities of carbon than their recent counterparts. The quantities of Ca2+, Mg2+ and K+were larger in the ancient woods except where prior cultivation had taken place. Total and organic phosphate contents of the ancient woodland soils were also consistently larger. The nature and pattern of soil variability in ancient woodland soils was quite distinct from that found in recent woods. Overall, the variability of soil acidity, carbon content and organic phosphate was larger in the ancient woodland soils but the pattern of variability differed between the soil properties. No clear association existed between the pattern of soil acidity and individual trees. At the surface of some of the woodland soils, however, carbon distribution appeared to be associated with individual tress. At depth in the ancien woodland soils, the association with the existing vegetation cover was not so clear. It is probable that the ancient woodland soils retained relict features of previous vegetation cover. Organic phosphate distribution was very strongly associated with the present vegetation cover. The pattern of distribution of organic phosphate appeared to be stronger than that of soil acidity and carbon content.
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Total and organic phosphate contents of the ancient woodland soils were also consistently larger. The nature and pattern of soil variability in ancient woodland soils was quite distinct from that found in recent woods. Overall, the variability of soil acidity, carbon content and organic phosphate was larger in the ancient woodland soils but the pattern of variability differed between the soil properties. No clear association existed between the pattern of soil acidity and individual trees. At the surface of some of the woodland soils, however, carbon distribution appeared to be associated with individual tress. At depth in the ancien woodland soils, the association with the existing vegetation cover was not so clear. It is probable that the ancient woodland soils retained relict features of previous vegetation cover. Organic phosphate distribution was very strongly associated with the present vegetation cover. 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R.</creatorcontrib><creatorcontrib>Moffat, A. J.</creatorcontrib><creatorcontrib>Nortcliff, S.</creatorcontrib><title>The nature of three ancient woodland soils in southern England</title><title>Journal of biogeography</title><description>Despite a wealth of published research on the nature of woodland soils, little is known about the nature of soils on sites that have supported woodland for many hundreds of years, namely ancient woodland. The properties and variability of soils in three ancient woods; one in the New Forest, Hampshire and two in Berkshire, were compared with those under recent woods. The acidity of ancient and recent woodland soils was high and remarkably similar. Only where cultivation of soils had preceded woodland establishment was soil acidity lower. The quantity of carbon in the soils studied was inversely related to soil acidity and the ancient woods had accumulated larger quantities of carbon than their recent counterparts. The quantities of Ca2+, Mg2+ and K+were larger in the ancient woods except where prior cultivation had taken place. Total and organic phosphate contents of the ancient woodland soils were also consistently larger. The nature and pattern of soil variability in ancient woodland soils was quite distinct from that found in recent woods. Overall, the variability of soil acidity, carbon content and organic phosphate was larger in the ancient woodland soils but the pattern of variability differed between the soil properties. No clear association existed between the pattern of soil acidity and individual trees. At the surface of some of the woodland soils, however, carbon distribution appeared to be associated with individual tress. At depth in the ancien woodland soils, the association with the existing vegetation cover was not so clear. It is probable that the ancient woodland soils retained relict features of previous vegetation cover. Organic phosphate distribution was very strongly associated with the present vegetation cover. The pattern of distribution of organic phosphate appeared to be stronger than that of soil acidity and carbon content.</description><subject>Acid soils</subject><subject>Agricultural soils</subject><subject>Agrology</subject><subject>Ancient woodland</subject><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>Biological and medical sciences</subject><subject>England</subject><subject>Fern and Forest Patterns</subject><subject>Forest soils</subject><subject>Forestry</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>General forest ecology</subject><subject>Generalities. Production, biomass. Quality of wood and forest products. General forest ecology</subject><subject>Mineral soils</subject><subject>Organic soils</subject><subject>recent woodland</subject><subject>Soil organic matter</subject><subject>soil properties</subject><subject>Soil science</subject><subject>soil variability</subject><subject>Synecology</subject><subject>Terrestrial ecosystems</subject><subject>Woodland soils</subject><subject>Woodlands</subject><issn>0305-0270</issn><issn>1365-2699</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1997</creationdate><recordtype>article</recordtype><recordid>eNqVkFtLwzAYhoMoOA__wIsi4l3rl3MrKOjQqYiCTITdhKz96jprq0nH5r-3pWNem5sE3lN4CDmmENH2nM0jypUMmUqSiCaJjpopAGgRrbbIYCNtkwFwkCEwDbtkz_t5a0okFwNyOZ5hUNlm4TCo86CZOcTAVmmBVRMs6zorbZUFvi5KHxRV-1g0M3RVcFO9d8oB2clt6fFwfe-T19ub8fAufHwe3Q-vHsNUcCFCrVLGKYKY2thKrTAVguWQ5Vxl0irkoDGLp6AzyXPGFOgELWaW8ZhPc5vxfXLa9365-nuBvjGfhU-xbP-A9cIbqtoKQVlrPO-Nqau9d5ibL1d8WvdjKJgOmZmbjovpuJgOmVkjM6s2fLJesT61Ze46EH7TwECKBLqNi962LEr8-ceAebi-16LNH_X5uW9q91cfC0Xjrj7s5cI3uNrI1n0YpbmW5u1pZF7GMUzkRBjNfwHda5hw</recordid><startdate>199709</startdate><enddate>199709</enddate><creator>Wilson, B. 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General forest ecology</topic><topic>Mineral soils</topic><topic>Organic soils</topic><topic>recent woodland</topic><topic>Soil organic matter</topic><topic>soil properties</topic><topic>Soil science</topic><topic>soil variability</topic><topic>Synecology</topic><topic>Terrestrial ecosystems</topic><topic>Woodland soils</topic><topic>Woodlands</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wilson, B. R.</creatorcontrib><creatorcontrib>Moffat, A. J.</creatorcontrib><creatorcontrib>Nortcliff, S.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Journal of biogeography</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wilson, B. R.</au><au>Moffat, A. J.</au><au>Nortcliff, S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The nature of three ancient woodland soils in southern England</atitle><jtitle>Journal of biogeography</jtitle><date>1997-09</date><risdate>1997</risdate><volume>24</volume><issue>5</issue><spage>633</spage><epage>646</epage><pages>633-646</pages><issn>0305-0270</issn><eissn>1365-2699</eissn><coden>JBIODN</coden><abstract>Despite a wealth of published research on the nature of woodland soils, little is known about the nature of soils on sites that have supported woodland for many hundreds of years, namely ancient woodland. The properties and variability of soils in three ancient woods; one in the New Forest, Hampshire and two in Berkshire, were compared with those under recent woods. The acidity of ancient and recent woodland soils was high and remarkably similar. Only where cultivation of soils had preceded woodland establishment was soil acidity lower. The quantity of carbon in the soils studied was inversely related to soil acidity and the ancient woods had accumulated larger quantities of carbon than their recent counterparts. The quantities of Ca2+, Mg2+ and K+were larger in the ancient woods except where prior cultivation had taken place. Total and organic phosphate contents of the ancient woodland soils were also consistently larger. The nature and pattern of soil variability in ancient woodland soils was quite distinct from that found in recent woods. Overall, the variability of soil acidity, carbon content and organic phosphate was larger in the ancient woodland soils but the pattern of variability differed between the soil properties. No clear association existed between the pattern of soil acidity and individual trees. At the surface of some of the woodland soils, however, carbon distribution appeared to be associated with individual tress. At depth in the ancien woodland soils, the association with the existing vegetation cover was not so clear. It is probable that the ancient woodland soils retained relict features of previous vegetation cover. Organic phosphate distribution was very strongly associated with the present vegetation cover. The pattern of distribution of organic phosphate appeared to be stronger than that of soil acidity and carbon content.</abstract><cop>Oxford, UK</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1111/j.1365-2699.1997.tb00074.x</doi><tpages>14</tpages></addata></record>
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subjects Acid soils
Agricultural soils
Agrology
Ancient woodland
Animal and plant ecology
Animal, plant and microbial ecology
Biological and medical sciences
England
Fern and Forest Patterns
Forest soils
Forestry
Fundamental and applied biological sciences. Psychology
General forest ecology
Generalities. Production, biomass. Quality of wood and forest products. General forest ecology
Mineral soils
Organic soils
recent woodland
Soil organic matter
soil properties
Soil science
soil variability
Synecology
Terrestrial ecosystems
Woodland soils
Woodlands
title The nature of three ancient woodland soils in southern England
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