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林分密度对韩国赤松林土壤 CO2 排放的影响。

Influence of stand density on soil CO2 efflux for a Pinus densiflora forest in Korea.

机构信息

Division of Environmental Science and Ecological Engineering, Korea University, Anam-dong, Seongbuk-gu, Seoul, 136-713, Korea.

出版信息

J Plant Res. 2010 Jul;123(4):411-9. doi: 10.1007/s10265-010-0331-8. Epub 2010 Apr 8.

Abstract

We investigated the influence of stand density [938 tree ha(-1) for high stand density (HD), 600 tree ha(-1) for medium stand density (MD), and 375 tree ha(-1) for low stand density (LD)] on soil CO(2) efflux (R (S)) in a 70-year-old natural Pinus densiflora S. et Z. forest in central Korea. Concurrent with R (S) measurements, we measured litterfall, total belowground carbon allocation (TBCA), leaf area index (LAI), soil temperature (ST), soil water content (SWC), and soil nitrogen (N) concentration over a 2-year period. The R (S) (t C ha(-1) year(-1)) and leaf litterfall (t C ha(-1) year(-1)) values varied with stand density: 6.21 and 2.03 for HD, 7.45 and 2.37 for MD, and 6.96 and 2.23 for LD, respectively. In addition, R (S) was correlated with ST (R (2) = 0.77-0.80, P < 0.001) and SWC (R (2) = 0.31-0.35, P < 0.001). It appeared that stand density influenced R (S) via changes in leaf litterfall, LAI and SWC. Leaf litterfall (R (2) = 0.71), TBCA (R (2) = 0.64-0.87), and total soil N contents in 2007 (R (2) = 0.94) explained a significant amount of the variance in R (S) (P < 0.01). The current study showed that stand density is one of the key factors influencing R (S) due to the changing biophysical and environmental factors in P. densiflora.

摘要

我们研究了立木密度(高立木密度为 938 株/公顷,中立木密度为 600 株/公顷,低立木密度为 375 株/公顷)对韩国中部一个 70 年生天然赤松人工林土壤 CO2 排放(R(S))的影响。在进行 R(S)测量的同时,我们还测量了凋落物量、总地下碳分配(TBCA)、叶面积指数(LAI)、土壤温度(ST)、土壤水分含量(SWC)和土壤氮(N)浓度,历时 2 年。R(S)(t C ha(-1) year(-1))和叶凋落物量(t C ha(-1) year(-1))随立木密度的变化而变化:高密度分别为 6.21 和 2.03,中密度分别为 7.45 和 2.37,低密度分别为 6.96 和 2.23。此外,R(S)与 ST(R (2) = 0.77-0.80,P < 0.001)和 SWC(R (2) = 0.31-0.35,P < 0.001)呈正相关。似乎立木密度通过凋落物量、LAI 和 SWC 的变化来影响 R(S)。凋落物量(R (2) = 0.71)、TBCA(R (2) = 0.64-0.87)和 2007 年总土壤 N 含量(R (2) = 0.94)解释了 R(S)变化的很大一部分(P < 0.01)。本研究表明,由于赤松的生物物理和环境因素不断变化,立木密度是影响 R(S)的关键因素之一。

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