中国科学院机构知识库网格系统: Changes of soil phosphorus speciation along a 120-year soil chronosequence in the Hailuogou Glacier retreat area (Gongga Mountain, SW China)

Changes of soil phosphorus speciation along a 120-year soil chronosequence in the Hailuogou Glacier retreat area (Gongga Mountain, SW China)

文献类型：期刊论文


作者	Zhou Jun1,2 ; Wu Yanhong1 ; Joerg, Prietzel 3; Bing Haijian1 ; Yu Dong1 ; Sun Shouqin1 ; Luo, Ji1 ; Sun Hongyang1,2
刊名	GEODERMA
出版日期	2013-03-01
卷号	195 期号:3 页码:251-259
关键词	Bioavailable P P fractionation Microbial P Biomass P Glacial retreat area Chronosequence
ISSN号	0016-7061
通讯作者	Wu Yanhong
合作状况	国际
中文摘要	The Hailuogou Glacier (Gongga Mountain, SW China) has been retreating in response to global warming. A soil chronosequence (Hailuogou Chronosequence) has developed in the retreat area, and a primary plant succession has developed on it. To investigate the changes of soil phosphorus (P) fractions along the young soil chronosequence in the cold and humid climate, soil samples were collected at seven sites of different ages (0 to 120 years). In all soil samples, concentrations of total P and of different P fractions (Bioavailable P, Al/Fe-bound P (P bound by Al and Fe oxides or hydroxides), Ca-bound P, and residual P) were determined using a sequential extraction technique. Organic P was determined using the high temperature ignition method. For the youngest (0 years, 12 years) soils, P forms were dominated by residual P, and topsoil forms of Ca-bound P, Al/Fe-bound P, organic P, microbial biomass P and bioavailable P were less than 1.86%. From 30 to 120 years, for the topsoil, concentrations of Ca-bound P and organic P gradually increased; the concentration of bioavailable P in surface soil also showed a trend of increase, with percentages of 5–11.5% to total soil P; the concentration of residual P decreased; the concentration of Fe/Al-bound P contributed less than 5% to total soil P at all sites. Ca-bound P and organic P were the dominant P fractions at the older sites (ages: 80 and 120 years). Soil P bioavailability and solubility were influenced by the changes of pH, and concentrations of Fe and Al oxide and hydroxide. The variations of vegetation and microbial activity are also considered as the impact factors of soil P forms. In the later stage of soil development (80 ~ 120 years), plenty of soil P was transformed into biomass P pool (299.3 kg ha^− 1).
英文摘要	The Hailuogou Glacier (Gongga Mountain, SW China) has been retreating in response to global warming. A soil chronosequence (Hailuogou Chronosequence) has developed in the retreat area, and a primary plant succession has developed on it. To investigate the changes of soil phosphorus (P) fractions along the young soil chronosequence in the cold and humid climate, soil samples were collected at seven sites of different ages (0 to 120 years). In all soil samples, concentrations of total P and of different P fractions (Bioavailable P, Al/Fe-bound P (P bound by Al and Fe oxides or hydroxides), Ca-bound P, and residual P) were determined using a sequential extraction technique. Organic P was determined using the high temperature ignition method. For the youngest (0 years, 12 years) soils, P forms were dominated by residual P, and topsoil forms of Ca-bound P, Al/Fe-bound P, organic P, microbial biomass P and bioavailable P were less than 1.86%. From 30 to 120 years, for the topsoil, concentrations of Ca-bound P and organic P gradually increased; the concentration of bioavailable Pin surface soil also showed a trend of increase, with percentages of 5-11.5% to total soil P; the concentration of residual P decreased; the concentration of Fe/Al-bound P contributed less than 5% to total soil P at all sites. Ca-bound P and organic P were the dominant P fractions at the older sites (ages: 80 and 120 years). Soil P bioavailability and solubility were influenced by the changes of pH, and concentrations of Fe and Al oxide and hydroxide. The variations of vegetation and microbial activity are also considered as the impact factors of soil P forms. In the later stage of soil development (80-120 years), plenty of soil P was transformed into biomass P pool (2993 kg ha(-1)). (c) 2012 Elsevier B.V. All rights reserved.
WOS标题词	Science & Technology ; Life Sciences & Biomedicine
学科主题	自然地理学 ; 土壤学 ; 环境学
类目[WOS]	Soil Science
研究领域[WOS]	Agriculture
关键词[WOS]	ORGANIC PHOSPHORUS ; NUTRIENT LIMITATION ; EXTRACTION METHOD ; NITROGEN ; PEDOGENESIS ; ECOSYSTEM ; TRANSFORMATIONS ; MICROORGANISMS ; AVAILABILITY ; PRODUCTIVITY
收录类别	SCI
语种	英语
WOS记录号	WOS:000316307200026
公开日期	2013-01-16
源URL	[http://192.168.143.20:8080/handle/131551/4814]
专题	成都山地灾害与环境研究所_山地表生过程与生态调控重点实验室
作者单位	1.Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Surface Proc & Ecol Regulat, Chengdu 610041, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.Tech Univ Munich, Lehrstuhl Bodenkunde, D-85350 Freising Weihenstephan, Germany
推荐引用方式 GB/T 7714	Zhou Jun,Wu Yanhong,Joerg, Prietzel,et al. Changes of soil phosphorus speciation along a 120-year soil chronosequence in the Hailuogou Glacier retreat area (Gongga Mountain, SW China)[J]. GEODERMA,2013,195(3):251-259.
APA	Zhou Jun.,Wu Yanhong.,Joerg, Prietzel.,Bing Haijian.,Yu Dong.,...&Sun Hongyang.(2013).Changes of soil phosphorus speciation along a 120-year soil chronosequence in the Hailuogou Glacier retreat area (Gongga Mountain, SW China).GEODERMA,195(3),251-259.
MLA	Zhou Jun,et al."Changes of soil phosphorus speciation along a 120-year soil chronosequence in the Hailuogou Glacier retreat area (Gongga Mountain, SW China)".GEODERMA 195.3(2013):251-259.

入库方式： OAI收割

来源：成都山地灾害与环境研究所

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Changes of soil phosphorus speciation along a 120-year soil chronosequence in the Hailuogou Glacier retreat area (Gongga Mountain, SW China)

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