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首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Effects of volcanic ash chemistry and former agricultural use on the soils and vegetation of naturally regenerated woodlands in the Massif Central, France
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Effects of volcanic ash chemistry and former agricultural use on the soils and vegetation of naturally regenerated woodlands in the Massif Central, France

机译:火山灰化学物质和以前的农业利用对法国Massif Central中天然更新林地的土壤和植被的影响

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摘要

In the Chaine des Puys, a volcanic mountain range in the French Massif Central, stands of silver birch and Scots pine have naturally regenerated during the past five decades. The woodlands have developed on former croplands, pastures and beathlands. Soil properties, species composition and dendrometric stand characteristics were investigated at sites of similar altitude and topographic conditions. Soils from the southern and northern parts of the study area differ in volcanic ash composition. Those of the nor-them part are afforested by birch and have developed mainly on trachytic ash; they have lower pH values and show accumulation of Fe-Al organic complexes. Soils of the southern part, afforested by Scots pine, are mostly on basaltic ash and have a higher pH, much less organic matter and more allophane. Soils of former croplands have lower C/N ratios, higher delta(15)N contents and greater potential N mineralization than those of former heathlands and pastures. The flora of the birch woodlands differs from that of the Scots pine woodlands and also varies with former land use, mainly because of different N availabilities. Woodlands established on former heathlands and pastures were more dense but less mature than stands on former croplands. Volcanic ash chemistry and the intensity of former agricultural use are key factors influencing present soil fertility, plant composition and stand development
机译:在法国地块中部的火山山脉Chaine des Puys,在过去的五十年中自然恢复了白桦林和苏格兰松树的林分。林地在以前的农田,牧场和荒地上发展。在相似的海拔和地形条件下,研究了土壤特性,物种组成和树木密度的特征。研究区南部和北部的土壤火山灰成分不同。普通部分的部分被桦树所绿化,主要以松散灰的形式发育。它们的pH值较低,并显示出Fe-Al有机配合物的积累。南部的土壤被苏格兰松树所绿化,主要是玄武灰,pH值较高,有机质少得多,而Allophane则多。与以前的荒地和牧场相比,以前的农田的土壤具有较低的C / N比,较高的delta(15)N含量和更大的潜在N矿化作用。桦木林地的植物区系与苏格兰松林地的植物区系不同,并且也随着以前的土地用途而变化,这主要是因为氮素利用率不同。建立在前荒地和牧场上的林地比以前耕地上的林地更茂密,但成熟程度较低。火山灰化学性质和以前的农业利用强度是影响目前土壤肥力,植物组成和林分发育的关键因素

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