Concurrent changes in soil inorganic and organic carbon during the development of larch, Larix gmelinii, plantations and their effects on soil physicochemical properties
Concurrent changes in soil inorganic and organic carbon during the development of larch, Larix gmelinii, plantations and their effects on soil physicochemical properties
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落叶松、落叶松、人工林发育过程中土壤无机碳和有机碳的同步变化及其对土壤理化性质的影响
DOI:
10.1007/s12665-012-1990-7
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发表时间:
2013-07
影响因子:
2.8
通讯作者:
Zu, Yuangang
中科院分区:
文献类型:
--
作者:
Wang, Hongyan;An, Jing;Zheng, Guangyu;Zu, Yuangang
Soil inorganic carbon (SIC) and organic carbon (SOC) levels can change with forest development, however, concurrent changes in soil carbon balance and their functional differences in regulating soil properties are unclear. Here, SIC, SOC, and other physicochemical properties of soil (N, alkali-hydrolyzed N, effective Si, electrical conductivity, pH, and bulk density) in 49 chronosequence plots of larch plantation forests were evaluated, by analyzing the concurrent changes in SIC and SOC storage during growth of plantation and the functional difference of these levels in maintaining soil sustainability. These soils had characteristically high SOC (15.34 kg m−2) and low SIC storage (83.38 g m−2 on average). Further, 28 of 30 linear regressions between SIC and SOC storage and larch growth parameters (age, tree size, and biomass density) were not statistically significant (p > 0.05). However, significant changes were observed in ratios of SIC and SOC with these growth parameters (between 0–40 cm and 40–80 cm, respectively; p < 0.05). These results were more useful for determining the changes in SIC and SOC vertical distribution than changes in storage. Moreover, larch growth generally decreased SIC and increased SOC. Linear correlation and multiple-regression analysis showed that the SIC influences soil acidity, whereas SOC affects soil nitrogen. This clearly indicates that larch growth could result in divergent changes in SIC and SOC levels, particularly in their vertical distribution; further, changes in SIC and SOC may variably affect soil physicochemical properties.
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DOI:
10.5860/choice.31-3799
发表时间:
2013-01
期刊:
--
影响因子:
--
作者:
S. Pal
通讯作者:
S. Pal
DOI:
--
发表时间:
1999
期刊:
--
影响因子:
--
作者:
Li Xuyon
通讯作者:
Li Xuyon
影响因子:
6.6
作者:
Sartori, Fabio;Lal, Rattan;Eaton, James A.
通讯作者:
Eaton, James A.
影响因子:
2.7
作者:
S. Singh;Ashutosh Kumar Singh;B. Sharma;J. C. Tarafdar
通讯作者:
S. Singh;Ashutosh Kumar Singh;B. Sharma;J. C. Tarafdar
影响因子:
1.5
作者:
W. J. Wang;Y. Zu;Hui Wang;T. Hirano;K. Takagi;K. Sasa;T. Koike
通讯作者:
W. J. Wang;Y. Zu;Hui Wang;T. Hirano;K. Takagi;K. Sasa;T. Koike