首页> 外文期刊>Journal of Vegetation Science >Litter quality effects of beech and hornbeam on undergrowth species diversity in Luxembourg forests on limestone and decalcified marl
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Litter quality effects of beech and hornbeam on undergrowth species diversity in Luxembourg forests on limestone and decalcified marl

机译:石灰石和脱钙泥灰对卢森堡森林中山毛榉和角树凋落物质量的影响对林下树种多样性的影响

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QuestionDo beech and hornbeam differ in undergrowth species diversity, and could these differences be explained by mass of the organic layer, pH or soil moisture? Could species richness under beech and hornbeam be explained by differences in N dynamics?LocationAncient forests dominated by beech and hornbeam in Luxembourg, on decalcified and lime-rich parent material.MethodsSpecies composition and soil characteristics, i.e. mass of the organic layer, pH, moisture content, bulk density and air-filled pore space, were determined under beech and hornbeam on decalcified marl and limestone, and analysed with cluster analysis, correspondence analysis and ANOVA, with tree species and parent material as independent factors. Net N mineralization, nitrification and N in soil and microbial biomass were determined in a laboratory incubation experiment over a pH gradient, and correlated with species richness.ResultsSpecies richness was lower under beech than under hornbeam on both decalcified marl and on limestone. Mass of the organic layer was higher under beech in all cases, but pH and soil moisture only differed between tree species on decalcified marl. Species richness increased with soil N, microbial N and nitrification in the mineral topsoil, but was not correlated with net N mineralization, and was negatively correlated with nitrification in the organic layer and with efficiency of N mineralization per unit microbe.ConclusionLitter quality affected species richness on both limestone and decalcified marl via the organic layer, but only on decalcified marl in terms of pH or soil moisture. Species richness did not seem to be stimulated by high overall net N mineralization or high nitrate availability in the organic layer, but only by high nitrate in the mineral topsoil.
机译:问题山毛榉和角树的林下物种多样性是否存在差异,这些差异能否用有机层的质量,pH值或土壤湿度来解释?可以通过氮动力学的差异来解释山毛榉和角树下的物种丰富度吗?位置在脱钙且富含石灰的母体上,卢森堡的山毛榉和角树为主导的古老森林。方法物种组成和土壤特征,即有机层的质量,pH,湿度在山毛榉和角树下,在脱钙的泥灰岩和石灰石上测定其含量,体积密度和充气孔隙空间,并以聚类分析,对应分析和ANOVA进行分析,以树种和母本为独立因素。在实验室温育实验中,在pH梯度上测定了土壤和微生物生物量中的净氮矿化,硝化作用和氮含量,并与物种丰富度相关。在所有情况下,山毛榉下的有机层质量都较高,但是在脱钙的泥灰岩上,pH和土壤水分仅在树种之间有所不同。物种丰富度随着土壤氮,微生物氮和矿物表层土壤中硝化作用的增加而增加,但与净氮矿化作用无关,与有机层中硝化作用和每单位微生物氮矿化效率呈负相关。通过有机层在石灰石和脱钙的泥灰土上都存在,但就pH或土壤湿度而言仅在脱钙的泥土上。总体净净氮矿化程度高或有机层中硝酸盐利用率高,似乎不会刺激物种丰富度,而矿物表层土壤中的硝酸盐含量高却不会刺激物种丰富度。

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