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Spatial patterns of fine root biomass and performances of understory dwarf bamboo and trees along with the gradient of soil N availability in broad-leaved natural forests and larch plantation

机译:阔叶天然林和落叶松人工林细根生物量的空间格局,矮矮竹和乔木的性能以及土壤氮素利用的梯度

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The importance of fine roots in forest ecosystem processes is well known. However, the contribution of understory vegetation to underground ecosystem processes is not well understood. We tested the hypothesis that fine-root biomass (FRB) and performance of the overstory and understory independently decrease with increasing soil N availability in cool-temperate deciduous broad-leaved natural forests and larch plantations in Japan. The mean contribution of understory FRB to total FRB (tree + understory) ranged from 4% to 78% (mean 37%). Tree FRB was negatively correlated with understory FRB, and understory FRB was dominant to tree FRB in infertile soil. Understory and total FRB were negatively correlated with soil net N mineralization rate, whereas tree FRB showed a quadratic relationship with soil N mineralization rate with the peak observed at mineralization of 58.4 kg N ha-1 y-1. The low tree FRB at infertile sites may be due to a belowground competitive effect of understory fine roots on tree FRB. Understory fine-root nitrogen concentration (FRN) and leaf to fine-root (L/FR) ratio were positively correlated with N mineralization rate. However, tree L/FR was not significantly correlated, whereas tree FRN was positively correlated, with soil N mineralization rate, suggesting that the leaf production efficiency of trees might not increase even on infertile soil. We suggest that belowground processes of overstory trees might change depending on understory vegetation, and that understory vegetation might affect the fine roots of overstory trees, which did not increase mass allocation but increased N use efficiency under low FRN.
机译:细根在森林生态系统过程中的重要性是众所周知的。然而,人们还不太了解地下植被对地下生态系统过程的贡献。我们测试了以下假说:在日本的温带落叶阔叶天然林和落叶松人工林中,细根生物量(FRB)和林下和林下性能随土壤N利用率的增加而独立降低。林下FRB对总FRB(树+林下)的平均贡献为4%至78%(平均37%)。林木FRB与林下FRB呈负相关,在不孕土壤中林木FRB占主导地位。林下和总FRB与土壤净N矿化率呈负相关,而树木FRB与土壤N矿化率呈二次关系,在矿化时观测到的峰值为58.4 kg N ha -1 y -1 。不孕部位的低树FRB可能是由于地下细根对FRB的地下竞争作用所致。林下细根氮浓度(FRN)和叶细根氮比(L / FR)与氮矿化率呈正相关。然而,树木的L / FR没有显着的相关性,而树木的FRN与土壤氮的矿化率呈正相关,这表明即使在不肥沃的土壤上树木的叶片生产效率也可能不会增加。我们认为,林下树木的地下过程可能会根据林下植被而变化,并且林下植被可能会影响林下树木的细根,这在低FRN下不会增加质量分配,但会增加氮的利用效率。

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