[1]何清清,邴海健,吴艳宏*,等.海螺沟冰川退缩区土壤元素分布特征及影响因素[J].山地学报,2017,(05):698-708.[doi:10.16089/j.cnki.1008-2786.000269]
 HE Qingqing,BING Haijian,WU Yanhong*,et al.Distribution Characteristics and Influencing Factors of Soil Elements in the Retreated Area of Hailuogou Glacier, SW China[J].Mountain Research,2017,(05):698-708.[doi:10.16089/j.cnki.1008-2786.000269]
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海螺沟冰川退缩区土壤元素分布特征及影响因素()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2017年05期
页码:
698-708
栏目:
出版日期:
2017-09-30

文章信息/Info

Title:
Distribution Characteristics and Influencing Factors of Soil Elements in the Retreated Area of Hailuogou Glacier, SW China
文章编号:
1008-2786-(2017)5-698-11
作者:
何清清12邴海健1吴艳宏1*王吉鹏1周 俊1孙宏洋1祝 贺12
1.中国科学院、水利部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,成都 610041;
2.中国科学院大学,北京 100049
Author(s):
HE Qingqing12 BING Haijian1WU Yanhong1* WANG Jipeng1 ZHOU Jun1 SUN Hongyang1 ZHU He12
1.Key Laboratory of Mountain Surface Processes and Ecological Regulation,Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041;
2.University of Chinese Academy of Sciences, Beijing 100049
关键词:
元素 土壤发育 元素分布特征 冰川退缩区 贡嘎山
分类号:
K903
DOI:
10.16089/j.cnki.1008-2786.000269
文献标志码:
A
摘要:
土壤形成和发育过程中,元素的赋存特征对陆地生态系统的健康发育至关重要。本研究选择海螺沟冰川退缩区,按照土壤年龄设置了6个采样点(0,30,40,52,80和120年),调查了18种元素在O层(有机层)、A层(矿物质层)和C层(母质层)的分布特征,并分析了主要影响因素。结果显示,在海螺沟冰川退缩区C层土壤中所有元素的浓度变化不大,反映了母岩基质相对单一; 在表层土壤(O层和A层)中,Al、Ba、Ca、Cr、Cu、Fe、K、Mg、Mn、Na、Ni、Sr、Ti、V发生明显亏损,P和Zn次之,而Cd和Pb存在明显富集。随土壤发育和植被演替,大多数元素的亏损程度增加,特别在针叶林阶段明显高于植被演替前期。土壤风化、植物吸收和径流损失对大多数元素的亏损具有重要影响,而Cd和Pb的高度富集主要归因于大气沉降和植物的归还作用。

参考文献/References:

[1] NOGUÉS-BRAVO D, ARAúJO M B, ERREA M,et al.Exposure of global mountain systems to climate warming during the 21st Century [J].Global Environmental Change, 2007, 17(3): 420-428.
[2] WU Y H, ZHOU J, BING H J, et al.Rapid loss of phosphorus during early pedogenesis along a glacier retreat choronosequence, Gongga Mountain(SW China)[J].PeerJ, 2015, 3: e1377.
[3] ZHOU J, WU Y H, PRIETZEL J, 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: 251-259.
[4] WANG J P, WU Y H, ZHOU J, et al.Carbon demand drives microbial mineralization of organic phosphorus during the early stage of soil development [J].Biology and Fertility of Soils, 2016, 52(6): 825-839.
[5] HE L, TANG Y.Soil development along primary succession sequences on moraines of Hailuogou Glacier, Gongga Mountain, Sichuan, China [J].Catena, 2008, 72(2): 259-269.
[6] BING H J, WU Y H, ZHOU J, et al.Mobility and eco-risk of trace metals in soils at the Hailuogou Glacier foreland in eastern Tibetan Plateau [J].Environmental Science and Pollution Research, 2016, 23(6): 5721-32.
[7] PRIETZEL J, DüMIG A, WU Y H, et al.Synchrotron-based P K-edge XANES spectroscopy reveals rapid changes of phosphorus speciation in the topsoil of two glacier foreland chronosequences [J].Geochimica et Cosmochimica Acta, 2013,108:154-171.
[8] BEMASCONI S M, BAUDER A, BOURDON B, et al.Chemical and biological gradients along the Damma glacier soil chronosequence, Switzerland [J].Vadose Zone Journal, 2011, 10(3): 867-883.
[9] HINDSHAW R S, REYNOLDS B C, WIEDERHOLD J G, et al.Calcium isotopes in a proglacial weathering environment: Damma glacier, Switzerland [J].Geochimica et Cosmochimica Acta, 2011, 75(1): 106-118.
[10] WU Y H, LI W, ZHOU J, et al.Temperature and precipitation variations at two meteorological stations on eastern slope of Gongga Mountain, SW China in the past two decades [J].Journal of Mountain Science, 2013, 10(3): 370-377.
[11] WU Y H, PRIETZEL J, ZHOU J, et al.Soil phosphorus bioavailability assessed by XANES and Hedley sequential fractionation technique in a glacier foreland chronosequence in Gongga Mountain, Southwestern China [J].Science China Earth Sciences, 2014, 57(8): 1860-1868.
[12] 杨子江,邴海健,周俊,等.贡嘎山海螺沟冰川退缩区土壤序列矿物组成变化[J].土壤学报,2015,52(3):507-516 [YANG ZiJiang, BING HaiJian, ZHOU Jun, et al.Variation of mineral composition along the soil chronosequence at the Hailuogou glacier foreland of Gongga Moutain [J].Mountain Research, 2015, 3: 507-516]
[13] 王绍强,朱松丽,周成虎.中国土壤土层厚度的空间变异性特征[J].地理研究, 2001, 20(2): 161-169 [WANG Shaoqiang, ZHU Songli, ZHOU Chenghu.Characteristics of spatial variability of soil thickness in China [J].Geographical Research, 2001, 20(2): 161-169]
[14] 王博,夏敦胜,余晔,等.兰州市城区河道表层沉积物地球化学元素分布特征[J].中国沙漠, 2012, 32(1): 168-174 [WANG Bo, XIA Dunsheng,YU Ye, et al.Element characters of river sediment of urban area in Lanzhou city [J].Jouranal of desert research, 2012, 32(1): 168-174]
[15] ZHOU J, BING H J, WU Y H, et al.Rapid weathering processes of a 120-year-old chronosequence in the Hailuogou Glacier foreland, Mt.Gongga, SW China [J].Geoderma, 2016, 267: 78-91.
[16] TAMBURINI F, PFAHLER V, BUENEMANN E K, et al.Oxygen isotopes unravel the role of microorganisms in phosphate cycling in soils [J].Environmental Science & Technology, 2012, 46(11): 5956-5962.
[17] WALKER T, SYERS J.The fate of phosphorus during pedogenesis [J].Geoderma, 1976, 15(1): 1-19.
[18] WARDLE D A, WALKER L R, BARDGETT R D.Ecosystem properties and forest decline in contrasting long-term chronosequences [J].Science, 2004, 305(5683): 509-513.
[19] VITOUSEK P M, PORDER S, HOULTON B Z, et al.Terrestrial phosphorus limitation: mechanisms, implications, and nitrogen-phosphorus interactions [J].Ecological Applications, 2010, 20(1): 5-15.
[20] 国家环境保护局.GB 15618-1995土壤环境质量标准 [S].北京:中国标准出版社,1997.[ Environmental quality standard for soils [S].Standards Press of China.1997]
[21] WU Y H, BING H J, ZHOU J, et al.Atmospheric deposition of Cd accumulated in the montane soil, Gongga Mt., China [J].Jouranal of Soils and Sediments, 2011,11:940-946.
[22] BING H J, WU Y H, ZHOU J, et al.Atmospheric deposition of lead in remote high mountain of eastern Tibetan Plateau, China [J].Atmospheric Environment, 2014, 99: 425-435.
[23] NADYA T, YIGAL E, LUDWIK H, et al.The influence of rainfall on metal concentration and behavior in the soil [J].Geochimica et Cosmochimica Acta, 1999, 63(21): 3499-3511.
[24] VIG K, MEGHARAJ M, SETHUNATHAN N, et al.Bioavailability and toxicity of cadmium to microorganisms and their activities in soil: a review.Advances in Environmental Research, 2003, 8(1), 121-135.
[25] WIGGENHAUSER M, BIGALKE M, IMSENG M, et al.Cadmium isotope fractionation in soil-wheat systems.Environmental Science & Technology, 2016, 50(17): 9223-9231.
[26] FÖLLMI K B, HOSEIN R, ARN K, et al.Weathering and the mobility of phosphorus in the catchments and forefields of the Rho ^ne and Oberaar glaciers, central Switzerland: implications for the global phosphorus cycle on glacial-interglacial timescales.Geochimica et Cosmochimica Acta, 2009, 73(8): 2252-2282.
[27] WONGFUN N, GÖTZE J, FURRER G, et al.Effect of water regime and vegetation on initial granite weathering in a glacier forefield: Evidences from CL, SEM, and Nomarski DIC microscopy.Geoderma, 2013, 211-212: 116-127.
[28] TIPPER E T, LEMARCHAND E, HINDSHAW R S, et al.Seasonal sensitivity of weathering processes: hints from magnesium isotopes in a glacial stream.Chemical Geology, 2012, 312-313: 80-92.
[29] 罗辑, 程根伟, 李伟, 等.贡嘎山天然林营养元素生物循环特征[J].北京林业大学学报, 2005, 27(2): 13-17 [LUO Ji, CHENG Genwei, Li Wei, et al.Characteristics of nutrient biocycling of natural forests on the Gongga Mountain [J].Journal of Beijing Forestry University, 2005, 27(2): 13-17]
[30] AERTS R, CHAPIN F S.The mineral nutrition of wild plants revisited: a re-evaluation of processes and patterns.1999, 30: 1-67.
[31] 陶宝先, 张金池, 俞元春.南京近郊主要森林类型对土壤重金属的吸收与累积规律[J].环境化学, 2011, 30(2): 448-453 [TAO Baoxian, ZHANG Jinchi, YU Yuanchun.Absorption and accumulation of heavy metals by forest plants in the outskirts of Nanjing City[J].Environmental Chemistry, 2011, 30(2): 448-453]
[32] 盛华夏.九龙江口红树林湿地凋落物分解与重金属动态研究[D].厦门:厦门大学,2009 [SHENG Huaxia.Studies on dynamics of heavy metal with decomposition of litter fall in mangrove wetland at Jiulongjiang River Estuary[D].Xiamen, Xiamen University, 2009]

相似文献/References:

[1]姚天全,张世玉,赵恒康,等.哀牢山徐家坝地区土壤中12种元素的自然背景值[J].山地学报,1999,(03):84.

备注/Memo

备注/Memo:
收稿日期(Received date):2017-06-20; 改回日期(Accepted date): 2017-09-30
基金项目(Foundation item):国家自然科学基金项目(41630751; 41402313); 中国科学院山地表生过程与生态调控重点实验室开放基金项目; 中科院青年创新促进会人才项目[National Nature Science Foundation of China(41630751; 41402313); Key Laboratory of Mountain Surface Processes and Ecological Regulation,Chinese Academy of Sciences; Youth Innovation Promotion Association, Chinese Academy of Science.]
作者简介(Biography):何清清(1993-),女,四川成都人,博士研究生,主要从事生物地球化学研究 [He Qingqing,(1993-), female, born in Chengdu, Sichuan province, Ph.D candidate, interested in biogeochemistry] E-mail:hqq@imde.ac.cn
*通讯作者(Corresponding author):吴艳宏(1969-),男,博士,研究员,主要研究方向为生物地球化学 [Wu Yanhong(1969-), male, Ph.D., professor, specialized in biogeochemistry] E-mail:yhwu@imde.ac.cn
更新日期/Last Update: 2017-09-30