中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Rapid recuperation of soil nitrogen following agricultural abandonment in a karst area, southwest china

文献类型:期刊论文

作者Wen, Li1,2,3; Li, Dejun1,2; Yang, Liqiong1,2,3; Luo, Pan1,2,3; Chen, Hao1,2; Xiao, Kongcao1,2; Song, Tongqing1,2; Zhang, Wei1,2; He, Xunyang1,2; Chen, Hongsong1,2
刊名Biogeochemistry
出版日期2016-09-01
卷号129期号:3页码:341-354
ISSN号0168-2563
关键词Karst area Post-agriculture succession N accumulation N dynamics Soil n stock Ecological restoration
DOI10.1007/s10533-016-0235-3
通讯作者Li, dejun(dejunli@isa.ac.cn)
英文摘要Soil nitrogen (n) dynamics are crucial for ecosystem development and carbon sequestration. however, n dynamics during post-agriculture succession have not been well understood. here soil n dynamics during post-agriculture succession were investigated in a subtropical karst area, southwest china. the succession sequence includes grassland (similar to 10 years), shrubland (similar to 29 years), secondary forest (similar to 59 years) and primary forest with cropland as reference. the soil is calcareous lithosols. soil n stock (0-15 cm) in the cropland (335.2 +/- 55.1 g n m(-2)) was not significantly different from that in the grassland, but was elevated by 120 to 221 % in the later three succession stages. across the sequence, soil n accumulated with an average rate of 12.4 g n m(-2) yr(-1). soil n stock recovered to the primary forest level in about 67 years following agricultural abandonment. no3 (-) concentrations increased while nh4 (+) concentrations decreased with years following agricultural abandonment. high no3 (-) concentrations (66.5-120.9 mg n kg(-1)) may imply n saturation in the shrubland, secondary forest and primary forest. rates of net n mineralization and nitrification increased with succession. delta n-15 of soil, leaves and litter was significantly elevated in the later three succession stages relative to the grassland, indicating that the n cycle became more open with succession. n release from bedrock weathering was likely a potential n source in addition to atmospheric n deposition and biological n fixation. our study suggests that n would not be the limiting nutrient for secondary succession and ecological restoration in the karst region of southwest china.
WOS关键词FOREST ECOSYSTEM CARBON ; ORGANIC-CARBON ; LAND-USE ; SECONDARY FORESTS ; NUTRIENT DYNAMICS ; CENTRAL AMAZONIA ; GREEN PROGRAM ; FIXING TREES ; C-STOCKS ; N-STOCKS
WOS研究方向Environmental Sciences & Ecology ; Geology
WOS类目Environmental Sciences ; Geosciences, Multidisciplinary
语种英语
出版者SPRINGER
WOS记录号WOS:000383104700006
URI标识http://www.irgrid.ac.cn/handle/1471x/2376090
专题中国科学院大学
通讯作者Li, Dejun
作者单位1.Chinese Acad Sci, Inst Subtrop Agr, Key Lab Agroecol Proc Subtrop Reg, 644 Yuanda 2nd Rd, Changsha 410125, Hunan, Peoples R China
2.Chinese Acad Sci, Inst Subtrop Agr, Huanjiang Observat & Res Stn Karst Ecosyst, Huangjiang 547100, Guangxi, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Wen, Li,Li, Dejun,Yang, Liqiong,et al. Rapid recuperation of soil nitrogen following agricultural abandonment in a karst area, southwest china[J]. Biogeochemistry,2016,129(3):341-354.
APA Wen, Li.,Li, Dejun.,Yang, Liqiong.,Luo, Pan.,Chen, Hao.,...&Wang, Kelin.(2016).Rapid recuperation of soil nitrogen following agricultural abandonment in a karst area, southwest china.Biogeochemistry,129(3),341-354.
MLA Wen, Li,et al."Rapid recuperation of soil nitrogen following agricultural abandonment in a karst area, southwest china".Biogeochemistry 129.3(2016):341-354.

入库方式: iSwitch采集

来源:中国科学院大学

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。