Titlebook: Environmental Effects of Afforestation in North-Western Europe; From Field Observati Gerrit W. Heil,Bart Muys,Karin Hansen Book 2007 Spring

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Environmental Effects of Afforestation in North-Western Europe978-1-4020-4568-4Series ISSN 1875-1318 Series E-ISSN 1875-1326

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Gilbert Lefevre,Fran?ois Michon,Mouna Viprey rate and magnitude of carbon (C) sequestration in biomass and soils following afforestation of cropland. Two oak (.) and four Norway spruce (.) afforestation chronosequences (age range 1 to 90 years) were studied with respect to C sequestration in Denmark, Sweden and the Netherlands..Biomass C sequ

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Grundlagen der Kostenvergleichsrechnung, (chronosequences) in Sweden, Denmark and the Netherlands. Rainfall, throughfall, soil moisture contents and groundwater dynamics were monitored at two oak chronosequences and four spruce chronosequences during a period of one to two years. At all chronosequences, the hydrological fluxes were simula

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?konomie der Geschlechterdifferenz industry (NO.). The most important ammonia source is emission from animal manure. The extent of this emission depends on manure composition and meteorological conditions. After N is emitted (either as NH. or as NO.) it will be transported over short or long distances. Deposition rates vary with the

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?konomie der Hochschulforschungy a role in the development of the field layer in newly planted forests on former agricultural land. One important goal of afforestation is the development of a natural ecosystem with a valuable field layer..In the course of succession, open-canopy species are replaced by climax species with a dense

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Ursula Maier-Rabler,Erich Sutterlüttiy, nutrients and water in trees and soil organic matter. Modelled tree growth depends on physiological plant factors, the size of plant pools, such as foliage mass, environmental factors, such as temperature and rainfall, and the total amount and turn-over rates of soil organic matter, which drives

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Zwischenbilanz zum methodischen Vorgehenent of a simplified soil model, however, we used existing complex models to start with. This soil model includes all relevant processes in order to simulate the temporal trajectory of carbon (C) sequestrations, nitrate leaching and water recharge. The soil model was derived from the existing models