期刊
JOURNAL OF SOILS AND SEDIMENTS
卷 17, 期 9, 页码 2250-2256出版社
SPRINGER HEIDELBERG
DOI: 10.1007/s11368-016-1421-6
关键词
Carbon cycle; Evergreen broadleaf forest; Forest succession; Land-use and land-cover change; Soil organic carbon; Soil respiration
资金
- National Natural Science Foundation of China [31270517, 31470529]
- Zhejiang A & F University Research and Development Fund [2010FR097]
The purpose of this study was to better understand how both the content and flux of soil carbon respond to forest succession and anthropogenic management practices in forests in subtropical China. We assembled from the literature information on soil organic carbon (SOC) and soil respiration (Rs) covering the forest successional chronosequence from pioneer masson pine (Pinus massoniana) forest (MPF) to medium broadleaf and needleleaf mixed forest (BNMF) and the climax evergreen broadleaf forest (EBF), along with the two major forest plantation types found in subtropical China, Chinese fir (Cunninghamia lanceolata) forest (CFF) and Moso bamboo (Phyllostachys pubescens) forest (MBF). Both SOC and Rs increased along the forest successional gradient with the climax EBF having both the highest SOC content of 33.1 +/- 4.9 g C kg(-1)(mean +/- standard error) and the highest Rs rate of 46.8 +/- 3.0 t CO2 ha(-1) year(-1). It can be inferred that when EBF is converted to any of the other forest types, especially to MPF or CFF, both SOC content and Rs are likely to decline. Stand age did not significantly impact the SOC content or Rs rate in either types of plantation. Forest succession generally increases SOC content and Rs, and the conversion of natural forests to plantations decreases SOC content and Rs in subtropical China.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据