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Diversity did not influence soil water use of tree clusters in a temperate mixed forest

机译:温带混交林中多样性并未影响树丛的土壤水分利用

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Compared to monocultures, diverse ecosystems are often expected to show morecomprehensive resource use. However, with respect to diversity–soil-water-userelationships in forests, very little information is available. Weanalysed soil water uptake in 100 tree clusters differing in tree speciesdiversity and species composition in the Hainich forest in central Germany.The clusters contained all possible combinations of five broadleaved treespecies in one-, two- and three-species clusters (three diversity levels),replicated fourfold (20 one-species, 40 two-species and 40 three-species clusters).We estimated soil water uptake during a summer dry period in 0–0.3 m soildepth, based on throughfall and soil moisture measurements with a simplebudgeting approach. Throughout the whole vegetation period in 2009, soilwater uptake was additionally determined at a higher temporal resolution andalso for a greater part of the soil profile (0–0.7 m) on a subset of 16intensive clusters. During the dry spell, mean soil water uptake was1.9 ± 0.1 mm day−1 in 0–0.3 m (100 clusters) and 3.0 ± 0.5 mm day−1in 0–0.7 m soil depth (16 clusters), respectively.Besides a slightly higher water use of Fraxinus clusters, we could not detect anyeffects of species identity or diversity on cluster water use. We discussthat water use may indeed be a conservative process, that differences intree-species-specific traits may be compensated for by other factors such asherb layer coverage and tree spatial arrangement, and that diversity-drivendifferences in water use may arise only at a larger scale. We furtherconclude that with respect to stand water use "tree diversity'' alone isnot an appropriate simplification of the complex network of interactionsbetween species traits, stand properties and environmental conditions thathave varying influence on stand water use, both in space and time.
机译:与单一文化相比,人们通常期望多样化的生态系统显示更全面的资源利用。但是,关于森林中的多样性-土壤-水-水友好化,几乎没有任何信息。我们对德国中部海尼希森林中100种不同树种多样性和物种组成的树丛的土壤水分吸收进行了分析,这些树丛包含一,二和三树种群(三个多样性水平)中五种阔叶树种的所有可能组合,重复四倍(20种一物种,40种二物种和40种三物种簇)。我们基于通径和土壤水分测量(采用简单预算方法),估计了夏季干旱时期土壤深度在0-0.3 m的土壤吸水量。在2009年的整个植被期内,在16个集约群的子集上,还以较高的时间分辨率和较大的土壤剖面(0-0.7 m)确定了土壤吸水量。在干旱时期,平均土壤水分吸收为1.9±。 0.1 mm day -1 在0-0.3 m(100个簇)和3.0±在0-0.7 m的土壤深度(16个簇)中分别为0.5 mm day −1 。除了 Fraxinus 簇的耗水量稍高外,我们无法检测到物种的任何影响集群用水的特性或多样性。我们讨论了用水可能确实是一个保守的过程,树种特定性状的差异可能会通过其他因素(例如草药层覆盖率和树木空间布置)得到补偿,并且由用水驱动的多样性差异可能只会在更大范围内出现。我们进一步得出结论,就林分用水而言,单独的“树种多样性”并不能适当简化物种特征,林分特性和环境条件之间的相互作用的复杂网络,这些相互作用对林分用水在空间和时间上都有不同的影响。

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