[1] ABRIL J. Constraints on the use of 137Cs as a time-marker to support CRS and SIT chronologies[J]. Environmental Pollution, 2004,129(1):31-37.[2] HE Q,WALLING D E. Interpreting particle size effects in the adsorption of 137Cs and unsupported 210Pb by mineral soils and sediments[J]. Journal of Environmental Radioactivity,1996,30 (2):117-137.[3] 陶炳德,沙占江,郭丽霞,等. 137Cs 示踪法研究湟水上游和布哈 河下游区域土壤侵蚀强度[J]. 干旱区地理,2013,36(6):997- 1005.[TAO Bingde,SHA Zhanjiang,GUO Lixia,et al. 137Cs tracing technique to study soil erosion between upper Huangshui Basin and lower Buha River Basin[J]. Arid Land Geography, 2013,36(6):997-1005.][4] RITCHIE J C,MCHENRY J R. Application of radioactive fallout cesium-137 for measuring soil erosion and sediment accumulation rates and patterns:a review[J]. Journal of Environmental Quality,1990,19(2):215-233.[5] WALLING D E,HE Q. Use of fallout 137Cs in investigations of overbank sediment deposition on river floodplains[J]. Catena, 1997,29(3):263-282.[6] PARSONS A J,FOSTER I D L. What can we learn about soil erosion from the use of 137Cs[J]. Earth-Science Reviews,2011, 108(1):101-113.[7] UNSCEAR. Sources and effects of ionizing radiation[M]. New York:United Nations Publications,2000.[8] ZHANG Q,SINGH V P,LI J,et al. Spatio-temporal variations of precipitation extremes in Xinjiang,China[J]. Journal of hydrology, 2012,434-435:7-18.[9] 袁方策,杨发相. 新疆地貌的基本特征[J]. 干旱区地理,1990, 13(3):35-38.[YUAN Fangce,YANG Faxiang. The basic geomorphologic characteristics of Xinjiang,China[J]. Arid Land Geography,1990,13(3):35-38.][10] 李军,杨青,史玉光. 基于DEM的新疆降水量空间分布[J]. 干 旱区地理,2010,33(6):868-873.[LI Jun,YANG Qing,SHI Yuguang. Spatial distribution of precipitation using DEM in Xinjiang, China[J]. Arid Land Geography,2010,33(6):868-873.][11] 孙桂燕,郭玲鹏,常存,等. 新疆天山中段南北坡水储量变化对 比分析[J]. 干旱区地理,2016,39(2):254-264.[SUN Guiyan, GUO Lingpeng,CHANG Cun,et al. Contrast and analysis of water storage changes in the north slopes and south slopes of the central Tianshan Mountains in Xinjiang[J]. Arid Land Geography, 2016,39(2):254-264.][12] 沈永平,苏宏超,王国亚,等. 新疆冰川、积雪对气候变化的响应(I):水文效应[J]. 冰川冻土,2013,35(6):513-527.[SHEN Yongping,SU Hongchao,WANG Guoya,et al. The responses of glaciers and snow cover to climate change in Xinjiang(I):Hydrological effect[J]. Journal of Glaciology and Geocryology, 2013,35(6):513-527.][13] CHEN F,HUANG X,ZHANG J,et al. Humid little ice age in arid central Asia documented by Bosten Lake,Xinjiang,China[J]. Science in China Series D:Earth Sciences,2006,49(12):1280- 1290.[14] 张成君,曹洁,类延斌,等. 中国新疆博斯腾湖全新世沉积环境 年代学特征[J]. 沉积学报,2004,22(3):494-499.[ZHANG Chengjun,CAO Jie,LEI Yanbin,et al. The chronological characteristics of Bosten Lake Holocene sediment environment in Xinjiang, China[J]. Acta Sedimentologica Sinica,2004,22(3): 494-499.][15] 吴敬禄,刘建军,王苏民. 近1500 年来新疆艾比湖同位素记录 的气候环境演化特征[J]. 第四纪研究,2004,24(5):585-590.[WU Jinglu,LIU Jianjun,WANG Sumin. Climatic change record from stable isotopes in Lake Aibi,Xinjiang during the past 1500 years[J]. Quaternary Sciences,2004,24(5):585-590.][16] 金爱春,蒋庆丰,陈晔,等. 新疆乌伦古湖的210Pb、137Cs测年与现 代沉积速率[J]. 现代地质,2010,24(2):377-382.[JIN Aichun, JIANG Qingfeng,CHEN Ye,et al. 210Pb and 137Cs dating and modern sedimentation rate in the Wulungu Lake,Xinjiang[J]. Geoscience,2010,24(2):377-382.][17] MA L,WU J,ABUDUWAILI J,et al. Aeolian particle transport inferred using a ~150-year sediment record from Sayram Lake, arid northwest China[J]. Journal of Limnology,2015,74(3): 584-593.[18] MA L,WU J,ABUDUWAILI J. Climate and environmental changes over the past 150 years inferred from the sediments of Chaiwopu Lake,central Tianshan Mountains,northwest China[J]. International Journal of Earth Sciences,2013,102(3): 959-967.[19] JAPAN METEOROLOGICAL AGENCY(JMA). Bulletin of the Radioactivity vol.83[M]. Tokyo:JMA,2001:21.[20] ALVAREZ-IGLESIAS P,QUINTANA B,RUBIO B,et al. Sedimentation rates and trace metal input history in intertidal sediments from San Simón Bay(Ría de Vigo,NW Spain)derived from 210Pb and 137Cs chronology[J]. Journal of Environmental Radioactivity,2007,98(3):229-250.[21] LAN B,ZHANG D,YANG Y. Evolution of Lake Ailike(northern Xinjiang of China)during past 130 years inferred from diatom data[J]. Quaternary International,2016. DOI:10.1016/j. quaint.2016.11.014[22] 邢闪. 长寿命放射性核素239,240Pu 和129I 在环境中的示踪研究[D]. 西安:中国科学院地球环境研究所,2015.[XING Shan. Trace application of long-lived radionuclides 239,240Pu and 129I in the environment[D]. Xi'an:Institute of Earth Environment, CAS,2015.][23] OLIVIER S,BAJO S,FIFIELD L K,et al. Plutonium from global fallout recorded in an ice core from the Belukha Glacier,Siberian Altai[J]. Environmental Science & Technology,2004,38 (24):6507-6512.[24] WU F,ZHENG J,LIAO H,et al. Vertical distributions of plutonium and 137Cs in lacustrine sediments in northwestern China: quantifying sediment accumulation rates and source identifications[J]. Environmental Science & Technology,2010,44(8): 2911-2917.[25] LIAO H,BU W,ZHENG J,et al. Vertical distributions of radionuclides(239+240Pu,240Pu/239Pu,and 137Cs)in sediment cores of Lake Bosten in Northwestern China[J]. Environmental Science & Technology,2014,48:3840-3846.[26] SIGURGEIRSSON M,ARNALDS O,PALSSON S,et al. Radiocaesium fallout behaviour in volcanic soils in Iceland[J]. Journal of Environmental Radioactivity,2005,79(1):39-53.[27] BUNZL K,SCHIMMACK W,KREUTZER K,et al.Interception and retention of chernobyl-derived 134Cs,137Cs and 106Ru in a spruce stand[J]. Science of the Total Environment,1989,78: 77-87.[28] FRANCIS C,THORNES J. Runoff hydrographs from three Mediterranean vegetation cover types[M]// THOMES J B. Vegetation and erosion:Processes and environments,Chichester UK: Wiley and Sons Ltd,1990:363-384.[29] ZHANG W,ZHOU J,FENG G,et al. Characteristics of water erosion and conservation practice in arid regions of Central Asia:Xinjiang Province,China as an example[J]. International Soil andWater Conservation Research,2015,3(2):97-111.[30] 秦伯强. 气候变化及人类活动对乌伦古湖的影响分析[J]. 干旱 区地理,1992,15(1):10-16.[QIN Boqiang. Analysis the impact of climate change and human activity on the Lake Wulungu[J]. Arid Land Geography,1992,15(1):10-16.][31] 高华中,姚亦锋. 近50年来人类活动对博斯腾湖水位影响的量 化研究[J]. 地理科学,2005,25(3):305-309.[GAO Huazhong, YAO Yifeng. Quantitative effect of human activities on water level change of Bosten Lake in recent 50 years[J]. Scientia Geographica Sinica,2005,25(3):305-309.][32] 杨云良,阎顺,贾宝全,等. 艾比湖流域生态环境演变与人类活 动关系初探[J]. 生态学杂志,1996,15(6):43-49.[YANG Yunliang, YAN Shun,JIA Baoquan,et al. Preliminary study on the relationship between the environmental evolution and the human activity in the Aibi Lake area[J]. Chinese Journal of Ecology, 1996,15(6):43-49.][33] WEI W,CHEN L,FU B,et al. The effect of land uses and rainfall regimes on runoff and soil erosion in the semi-arid loess hilly area,China[J]. Journal of Hydrology,2007,335(3):247-258.[34] FU B J,NIU D,YU G R,et al. Application of landscape ecology in long term ecological research. In Landscape Ecological Applications in Man-Influenced Areas,Hong S K et al(eds.). Springer Netherlands,2008:33-56.[35] GOODBRED S L,KUEHL S A. Floodplain processes in the Bengal Basin and the storage of Ganges-Brahmaputra River sediment: an accretion study using 137Cs and 210Pb geochronology[J]. Sedimentary Geology,1998,121(3):239-258. |