Arid
DOI10.1016/j.geoderma.2008.02.004
Forms and profile distribution of soil phosphorus in four wetlands across gradients of sand desertification in Northeast China
Wang, Guo-Ping; Zhai, Zheng-Li; Liu, Jing-Shuang; Wang, Jin-Da
通讯作者Wang, Guo-Ping
来源期刊GEODERMA
ISSN0016-7061
出版年2008
卷号145期号:1-2页码:50-59
英文摘要

Little is known about the relationship between soil phosphorus (P) forms of semiarid wetlands and surrounding upland land-use patterns. Soil P in different depths of four wetlands was fractionated using a modified Hedley fraction method. The wetland soil cores were sampled along a gradient of sand desertification in the west of Songnen Plain (Northeast China), and sectioned with high-resolution (2-cm intervals). The soil total P (P-t) content and P forms varied significantly within and among the profiles with strongly alkaline (pH 7.9 to 10.5) in sand and no sand desertification wetlands. The Pt mean content ranged from 90.8 to 231.6 mg/kg in the sand desertification wetlands, and 421.3 mg/kg in the no sand desertification wetland. Dilute HCl extractable inorganic P (P) is the predominant form in all profiles, both as absolute values and as a percentage of total extracted Pi (mean: 56-77%), and concentrated HCl extractable organic P (P.) is the predominant form of total extracted Po (mean: 45-68%). Moreover, Dil.HCl-P-i and Conc.HCl-P-i were strongly positive correlated with the content of Al, Ca, Fe, clay and silt percentages, but negative correlated with sand percentages. All forms of organic P (NaHCO3-P-o, NaOH-P-o, and Conc.HCl-P-o) were strongly positive correlated with the content of total organic carbon (Core). In addition, for comparison of soil heterogeneity affected by sand desertification, uplands surface soil samples were collected from grassland, cultivated land, and sand lands surrounding the four representative wetlands. The results indicated that P forms of the surface soils were significantly different among studied upland land-use patterns. Consequently, there were general differences in soil P forms between sand and no sand desertification wetland profiles. The Residual-P heterogeneity in the wetland profiles can partly be attributed to the influences of different intensity of sand desertification. And Residual-P could be as an index of the intensity of desertification. (c) 2008 Elsevier B.V. All rights reserved.


英文关键词phosphorus forms soil sand desertification wetlands Songnen Plain
类型Article
语种英语
国家Peoples R China
收录类别SCI-E
WOS记录号WOS:000257019300006
WOS关键词FRESH-WATER WETLANDS ; XIANGHAI WETLANDS ; TRANSFORMATIONS ; PEDOGENESIS ; FRACTIONS ; RETENTION ; ECOSYSTEMS ; SEDIMENTS ; DYNAMICS ; RESPECT
WOS类目Soil Science
WOS研究方向Agriculture
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/157401
作者单位Chinese Acad Sci, NE Inst Geog & Agr Ecol, Key Lab Wetland Ecol & Environm, Changchun 130012, Peoples R China
推荐引用方式
GB/T 7714
Wang, Guo-Ping,Zhai, Zheng-Li,Liu, Jing-Shuang,et al. Forms and profile distribution of soil phosphorus in four wetlands across gradients of sand desertification in Northeast China[J],2008,145(1-2):50-59.
APA Wang, Guo-Ping,Zhai, Zheng-Li,Liu, Jing-Shuang,&Wang, Jin-Da.(2008).Forms and profile distribution of soil phosphorus in four wetlands across gradients of sand desertification in Northeast China.GEODERMA,145(1-2),50-59.
MLA Wang, Guo-Ping,et al."Forms and profile distribution of soil phosphorus in four wetlands across gradients of sand desertification in Northeast China".GEODERMA 145.1-2(2008):50-59.
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