Effects of harvest residue management on soil carbon and nitrogen processes in a Chinese fir plantation

被引:25
|
作者
Hu, Zhenhong [1 ,4 ]
He, Zongming [2 ]
Huang, Zhiqun [1 ]
Fan, Shaohui [3 ]
Yu, Zaipeng [1 ]
Wang, Minhuang [1 ]
Zhou, Xuhui [4 ]
Fang, Changming [4 ]
机构
[1] Fujian Normal Univ, Coll Geog Sci, Fuzhou 350007, Peoples R China
[2] Fujian Agr & Forestry Univ, Coll Forestry, Fuzhou 350002, Peoples R China
[3] Int Network Bamboo & Rattan INBAR, Beijing 100102, Peoples R China
[4] Fudan Univ, Coastal Ecosyst Res Stn Yangtze River Estuary, Inst Biodivers Sci, Minist Educ,Key Lab Biodivers Sci & Ecol Engn, Shanghai 200433, Peoples R China
基金
中国国家自然科学基金;
关键词
Cunninghamia lanceolata; Labile carbon pools; Soil carbon; Soil CO2 efflux; Subtropical China; PINUS-RADIATA PLANTATIONS; DIFFERENT N-STATUS; TEMPERATE FORESTS; CO2; EFFLUX; SUBTROPICAL AUSTRALIA; ORGANIC-MATTER; DIOXIDE FLUX; TREE GROWTH; RESPIRATION; STORAGE;
D O I
10.1016/j.foreco.2014.04.023
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Plantation management can affect ecosystem soil carbon (C) and nitrogen (N) cycles. However, how different harvest residue management strategies impact soil C and N processes over the long term is largely unclear. In this study, we examined effects of harvest residue management on soil C and N concentrations, labile soil C and N pools and soil CO2 efflux (Rs) at different stages after Chinese fir (Cunninghamia lanceolata) was replanted in subtropical China. The residue management treatments were slash and burning, whole-tree harvesting, stem-only harvesting and stem only harvesting with double residue retention. Our results showed that the harvest residue management treatments did not differ significantly in their effect on soil C and N, mineral N (NH4+-N plus NO3--N), dissolved organic C or total dissolved N concentrations, except for soil N concentrations in surface soil (0-10 cm) at year 3 and soil total dissolved N concentrations at year 12, which were significantly lower where the slash was burnt than in the double residue retention treatment. Similarly, Rs did not differ significantly among the four residue management strategies at year 15. Topsoil temperature and topsoil moisture were also unaffected by harvest residue management treatment. Soil temperature was found to be the most important factor controlling the temporal pattern of Rs, accounting for 65.8% of seasonal variation of Rs. There was no significant difference in temperature sensitivity of Rs (Q(10)) or annual Rs among the four treatments. These results indicated that harvest residue management may not significantly cause long-term effects on soil C cycling and N availability in subtropical Chinese fir plantations. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:163 / 170
页数:8
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