[1]陈思思,张虎才*,常凤琴,等.异龙湖湖泊沉积对流域人类活动的响应[J].山地学报,2016,(03):274-281.[doi:10.16089/j.cnki.1008-2786.000128]
　CHEN Sisi,ZHANG Hucai,CHANG Fengqin,et al.Human Activities Indicated by the Sediments at the Yilong Lake[J].Mountain Research,2016,(03):274-281.[doi:10.16089/j.cnki.1008-2786.000128]
点击复制

异龙湖湖泊沉积对流域人类活动的响应()
分享到：

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2016年03期
页码:
274-281
栏目:
山地生态和环境
出版日期:
2016-06-01

文章信息/Info

Title:
Human Activities Indicated by the Sediments at the Yilong Lake
文章编号:
1008-2786-(2016)3-274-08
作者:
陈思思; 张虎才*; 常凤琴; 吴 汉; 卢慧斌; 刘东升1
云南师范大学旅游与地理科学学院高原湖泊生态与全球变化重点实验室,高原地理过程与环境云南省重点实验室,云南 昆明 650500
Author(s):
CHEN Sisi; ZHANG Hucai; CHANG Fengqin; WU Han; LÜ Huibin;  LIU Dongsheng
Key Laboratory of Plateau Lake Ecology and Globe Change, Yunnan Provincial Key Laboratory of Plateau Geography Process and Environment Changes, College of Tourism and Geography Science, Yunnan Normal University, Kunming Chenggong 650500,China
关键词:
异龙湖;  粒度;  碳酸盐;  有机质;  人类活动
Keywords:
Yilong Lake;  grain size;  carbonate;  organic;  human activities
分类号:
P931.6,X144
DOI:
10.16089/j.cnki.1008-2786.000128
文献标志码:
A
摘要:
通过对异龙湖短钻岩芯沉积物粒度、碳酸盐以及有机质含量等环境代用指标研究,结合文献资料和当地气象数据并参考实验室其他项目组137Cs-210Pb方法建立的年代标尺,讨论了异龙湖流域1880年以来的环境变化和人类活动对湖泊沉积环境的影响。结果表明:岩芯35～25 cm段(1880—1936年)碳酸盐含量、中值粒径均值较高,表明这一时期为暖湿气候,TOC含量处于低值且平缓,证实人类活动对周围环境影响较小,湖泊环境变化的影响因素以自然因素为主; 至25～15 cm段(1936—1996年)碳酸盐含量明显下降,有机质含量快速增加,指示湖泊沉积环境受人类活动影响强烈,碳酸根离子等其他化合物含量、反应条件、过程及碳酸盐沉淀保存条件发生改变,在此种情况下,指标已不能指示湖泊环境变化; 岩芯15～0 cm段(1996—2013年)沉积物粘土含量升高,砂含量降低,应与异龙湖流域防护林工程有关,这一时期的指标特征表明人类活动强度较之前有所减弱,并且开始有意识地恢复流域生态。
Abstract:
The sediment core YLH-1 from the Yilong lake in Yunnan Province of China was analyzed for grain size,contents of carbonate and organic. Accurate sediment chronology was referred by YL-1 core's 210Pb and 137Cs. By comparing the grain-size, carbonate and organic proxies with documents and meteorological data, we discussed the environmental evolution and influence of human activities on depositional environment since 1880.Results show that both carbonate and average median grain-size high contents at 35～25 cm depth(1880—1936 a),the lake catchment was characterized of increased rainfall and relatively warm climate. During this period, in a low organic content, the lake evolution and the environmental change were mainly influenced by natural factors. At 25～15 cm depth(1936—1996 a)obviously lower carbonate content and organic content increased rapidly,with implied the sedimentary environment of the loke affected by human activities. Some properties of carbonate ions and other compounds, including the content, reaction condition, and the preservation condition of carbonate precipitations can vary. in this case, carbonate content could not be explained by temperature or precipitation change. The lake catchment was shelter forest project implementation and consciously ecological recovery. It may be why grain size in YLH-1 core became finer at 15～0 cm depth(1996—2013 a).

参考文献/References:

[1] Wasson R J. Land use and climate impacts on fluvial systems during the period of agriculture[M].PAGES Workshop Report,Series 96-2,1996:10-20
[2] Zhang H, Peng J, Ma Y, et al. Late Quaternary palaeolake levels in Tengger Desert, NW China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2004, 211:45-58
[3] Colmans M. Continental drilling for paleoclimate record[J]. Eos Trans, AGU, 1995, 76(37): 364
[4] 史正涛, 明庆忠, 张虎才. 云南高原典型湖泊演化及环境变化初步考察[J]. 地质力学学报, 2004, 10(4): 344-350[Shi Zhengtao, Ming Qingzhong, Zhang Hucai. Investigation of the evolution and environment change of typical lakes in Yunnan Province[J]. Journal of Geomechanics, 2004, 10(4): 344-350 ]
[5] 史正涛, 明庆忠, 张虎才. 云南高原典型湖泊现代过程及环境研究进展[J]. 云南地理环境研究, 2005, 17(1): 24-26[Shi Zhengtao, Ming Qingzhong, Zhang Hucai. A study review on the modern processes and environmental evolution of the typical lakes in Yunnan[J]. Yunnan Geographic Environment Research, 2005, 17(1): 24-26]
[6] Cui B, Zhai H. Characteristics of wetland functional degradation in plateau lake and its ecological water requirement for restoration[J].Chinese Sciences Bulletin, 2006, 51(Suppl.): 61-69
[7] 李晓杰. 石屏县异龙湖渔业产业发展现状及对策[J]. 现代农业科技, 2014,(3): 328-333[Li Xiaojie. Fisheries industry development present situation and the countermeasures in the Yilong Lake of ShiPing prefecture[J]. XianDai NongYe KeJi, 2014,(3): 328-333]
[8] 王忠泽. 云南省异龙湖藻类植物及鱼产力研究[J]. 水产学报, 1997, 21(1): 93-96[Wang Zhongze. Research of algae and fish productivity in the Yilong Lake,Yunnan[J]. Journal of Fisheries of China, 1997, 21(1): 93-96]
[9] 黄春兰, 蒙睿, 杨林,等. 异龙湖流域生态旅游开发初探[J]. 西南林学院学报, 2004, 24(3):29-31[Huang Chunlan, Meng Rui, Yang Lin, et al. A preliminary study on the ecotourism development in the Yilonghu Lake area[J]. Journal of southwest forestry college, 2004, 24(3):29-31]
[10] 仇国新. 石屏异龙湖区域环境与经济开发规划研究[J]. 云南环境科学,1997,(01): 9-14[Chou Guoxin. Research of environmental and economic development planning in Yi-Long lake area of Shiping prefecture[J]. Yunnan Environmental science,1997,(01): 9-14]
[11] 李沈丽. 异龙湖流域生态环境的综合治理[J]. 林业调查规划, 2009, 34(2): 108-110[Li Shenli. Ecological environmental integrated control for Yilonghu watershed[J]. Forest Inventory and Planning, 2009, 34(2): 108-110]
[12] 荆春燕, 曾广权. 异龙湖流域生态功能区划分析[J]. 云南环境科学,2003, 22(4): 49-51[Jing Chunyan, Zeng Guangquan. Analysis on ecological functional regionization in Yilong lake basin[J]. Yunnan Environmental science,2003, 22(4): 49-51]
[13] 刘晓海, 宁平, 张军莉,等. 围湖造田和退田还湖对异龙湖的影响[J]. 昆明理工大学学报(理工版), 2006, 31(5): 78-81[Liu Xiaohai, Ning Ping, Zhang Junli, et al. Towards the effects of reclaiming the land from the lake and restoring the lake from the land in Yilong lake[J]. Journal of Kunming University of Science and Technology( Science and Technology), 2006, 31(5): 78-81]
[14] 赵磊. 云南异龙湖生态系统稳态转换过程与关键灾变因子反演研究[D]. 北京: 中国科学院生态环境研究中心, 2013:28-38[Zhao Lei. The regime shifts and inversion of catastrophic driving factors in the ecosystems of Yilong lake, Yunnan[D]. Beijing:Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, 2013:28-38]
[15] 王苏民, 窦鸿身. 中国湖泊志[M]. 北京:科学出版社, 1998: 379-381[Wang Sumin, Dou Hongshen. Chinese lakes[M]. Beijing: Science Press, 1998: 379-381]
[16] 云南省石屏县志编纂委员会. 石屏县志[M]. 昆明:云南人民出版社,1990: 56-58[Yunnan Shiping County History Compilation Committee. Shiping county history[M]. Kunming:Yunnan People's Publishing House, 1990: 56-58]
[17] 张振克, 王苏民, 吴瑞金,等.全新世中期洱海湖泊沉积记录的环境演化与西南季风变迁[J]. 科学通报,1998,43(19): 2127-2128[Zhang Zhenke, Wang Sumin, Wu Ruijin, et al. Environmental evolution and southwest monsoon changes in mid-Holocene recorded by lake sediments in Erhai Lake[J]. Chinese Science Bulletin,1998, 43(19); 2127-2128]
[18] 雷国良, 张虎才, 张文翔,等. Mastersize2000型激光粒度仪分析数据可靠性检验及意义——以洛川剖面S4古土壤为例[J]. 沉积学报, 2006, 24(4): 531-539 [Lei Guoliang, Zhang Hucai, Zhang Wenxiang, et al. The reliability and significance of the grain- size obtained by mastersize 2000 laser analyzer:a case study on the typical S4 from Luochuan section[J]. Acta Sedimentologica Sinica, 2006, 24(4): 531-539]
[19] 陈敬安, 万国江, 张峰,等. 不同时间尺度下的湖泊沉积物环境记录——以沉积物粒度为例[J]. 中国科学(D辑), 2003, 33(6): 564-568[Chen Jingan, Wan Guojiang, Zhang Fang, et al. Environment record by lake sediments from different time scale:A case Study of sediment grain size as an example[J]. Science in China(Series D), 2003, 33(6):563-568]
[20] Celina Campell. Late Holocene lake sedimentology and climate change in southern Alberta, Canada[J]. Quaternary Research,1997(49): 96-101
[21] Vanniére B, Bossuet G. Walter-Simonnet AV, et al. Land use change, soil erosion and alluvial dynamic in the lower Doubs Valley over the 1st millennium AD(Neublans, Jura, France)[J]. Journal of Archaeological Science, 2003, 30(10): 1293-1299
[22] Zhang W, Zhang H, Ming Q, et al. Lake sediment records on climate change and human activities in the Xingyun Lake catchment, SW China [J/OL]. Plos One, 2014, 9(7).2015-02-13,http://xueshu.baidu.com/s?wd=paperuri%3A%28116463b3633 eeff11167618348377,Doi:10.137/journal.pone.0102167
[23] 莱尔曼主编. 王苏民等译. 湖泊的化学、地质学和物理学[M]. 北京:地质出版社1989:39-42[Lerman A. Translated by WANG Sumin. Lakes chemistry geology physics[M]. Beijing:Geological Publishing House, 1989:39-42]
[24] 曹洁, 张家武, 张成君, 等.青藏高原北缘哈拉湖近800年来湖泊沉积及其环境意义[J]. 第四纪研究, 2007, 27(1):100-107[Cao Jie, Zhang Jiawu, Zhang Chengjun, et al. Environmental changes during the past 800 years recorded in lake sediments from Hala lake on the northern Tibetan plateau[J]. Quaternary Science, 2007, 27(1):100-107]
[25] 陈敬安, 万国江, 汪福顺, 等. 湖泊现代沉积物碳环境记录研究[J]. 中国科学:D辑. 2002, 32(1):73-80[Chen Jing'an, Wan Guojiang, Wang Fushun, et al. Research of the carbon environment records in the lake modern sediments[J]. Science in China:Series D, 2002,32:73-80]
[26] Dean WE. The carbon cycle and biogeochemical dynamics in lake sediments[J]. Journal of Paleolimnology, 1999, 21: 375-393
[27] 周爱峰, 陈发虎, 强明瑞, 等. 内陆干旱区柴达木盆地苏干湖年纹层的发现及其意义[J]. 中国科学(D辑), 2007, 37(7):941-948[Zhou Aifeng, Chen Fahu, Qiang Mingrui, et al. The discovery of annually laminated sediments(varves)from shallow Sugan Lake in inland arid China and their paleoclimatic significance[J]. Science in China(Series D), 2007, 50(8): 1218-1224]
[28] 韦红波, 李锐, 杨勤科. 我国植被水土保持功能研究进展[J]. 植被生态学报, 2002, 26(4):48-49[Wei Hongbo, Li Rui, Yang Qinke.Research advances of vegetation effect on soil and water conservation in China[J]. Acta Phytoecologica Sinica, 2002, 26(4):48-49]

相似文献/References:

[1]白 雪,杨振京*,毕志伟,等.银川盆地第四纪沉积物粒度特征及其沉积环境[J].山地学报,2017,(06):874.[doi:10.16089/j.cnki.1008-2786.000289]
　BAI Xue,YANG Zhenjing,BI Zhiwei,et al.Grain Size Characteristics and Its Depositional Environmentof Quaternary Sediments in Yinchuan Plain, Northwest China[J].Mountain Research,2017,(03):874.[doi:10.16089/j.cnki.1008-2786.000289]
[2]文星跃,吴 勇,黄成敏,等.岷江上游晚更新世黄土粒度与元素组成特征及其物源指示意义[J].山地学报,2019,(04):488.[doi:10.16089/j.cnki.1008-2786.000441]
　WEN Xingyue,WU Yong,HUANG Chengmin,et al.Grain Size & Elements Composition Characteristics and Their Implications for Provenance of the Late Pleistocene Loess in the Upper Reaches of the Minjiang River,China[J].Mountain Research,2019,(03):488.[doi:10.16089/j.cnki.1008-2786.000441]
[3]邱 潇,涂国祥*,李 明,等.汉源九襄砾石层沉积特征及演化[J].山地学报,2020,(5):647.[doi:10.16089/j.cnki.1008-2786.000542]
　QIU Xiao,TU Guoxiang*,LI Ming,et al.Sedimentary Characteristics and Evolution of the Stratified Gravel Deposits in the Jiuxiang Area of Hanyuan, China[J].Mountain Research,2020,(03):647.[doi:10.16089/j.cnki.1008-2786.000542]

备注/Memo

备注/Memo:
收稿日期(Received date):2015-02-13; 修回日期(Accepted):2015-03-27。
基金项目(Foundation item):国家自然科学基金(41361008)、云南省高端人才引进项目(2010CI111)和湖泊沉积与环境变化云南省创新团队项目(2010CI)资助。[This study was funded by National Natural Science Foundation of China, No.41361008,and Yunnan Provincial Government Senior Talent Program(2010CI111)and The Innovation Team Project on Lake Ecology and Environmental Change of Yunnan(2011CI).]
作者简介(Biography):陈思思(1990-), 女, 汉族, 海南文昌人, 硕士研究生,研究方向为湖泊沉积与环境变化。 [Chen Sisi(1990-), female, master candidute, majored in lake sediments and environmental evolution.] E-mail: chensisi929@163.com
*通信作者(Corresponding author):张虎才(1962-), 男, 汉族, 陕西凤翔人, 博士生导师, 主要从事湖泊与环境变化研究。[Zhang Hucai(1962-), male, professor, mainly interested in lake sediments and environmental evolution.] E-mail: hucaizhang@yahoo.com
更新日期/Last Update: 2016-05-30