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黑龙江省五大连池近百年环境变化研究
  • ISSN号:1001-7410
  • 期刊名称:《第四纪研究》
  • 时间:0
  • 分类:P343.3[天文地球—水文科学;天文地球—地球物理学]
  • 作者机构:[1]中国科学院南京地理与湖泊研究所湖泊与环境国家重点实验室,南京210008, [2]中国科学院研究生院,北京100049
  • 相关基金:科技部基础性工作专项项目(批准号:2006FY110600)、国家自然科学基金项目(批准号:41072133)和中国科学院碳专项项目支持.致谢 感谢吴艳宏研究员、邴海健博士、陶井奎,哈尔滨师范大学肖海丰副教授等人在野外采样和实验分析中给予的帮助和支持,感谢广东省阳江市气象局吴长春工程师提供所需气象数据,同时也感谢五大连池管委会在采样过程中提供的帮助.
中文摘要:

2009年6月用重力采样器在黑龙江省五大连池的三池和五池分别采集岩芯钻孔(wdlc-3孔和wdlc-5孔),运用核素^210Pb和^137Cs进行定年,同时分析了岩芯沉积物的理化指标,包括烧失量(LOI550℃)、总磷(TP)、总氮(TN)、粒度、金属元素和磁化率,研究近代五大连池湖泊环境演化过程以及人类活动的影响。结果表明:1920s~1950s,湖泊沉积物中值粒径较大,LOI550℃和TN呈增长趋势,两孔Al和Fe含量呈增长趋势或处于高值阶段,可能与该期人类活动如开垦荒地有关;1950s~1980s,中值粒径较小或呈减少趋势,而TN,Al和Fe及重金属的含量呈增加趋势,人类活动如毁林、毁草开荒开始成为湖泊环境变化的主导因素;1980s~2000s阶段氮、磷增加更为迅速,重金属的含量也呈快速增长趋势,这可能与化肥、农药、含磷物品、含铅汽油的大量使用以及增强的工业活动有关;2000s以来,湖泊主要面临营养水平增加导致的富营养化问题。

英文摘要:

Wudalianchi Lake(48°40′N - 48°47′N, 126°06′E - 126°15′E) is located in Wudalianehi City, Heilongjiang Province, China. The lake is composed of five small lakes,with the third lake area being 8.2km^2 ,and the fifth lake area being 5.3km^2. Two sedimentary cores,named wdlc-3 and wdlc-5 ,were collected from the third and fifth lake (wdlc-3, 48°43′39.72″ N, 126°12′56.84″ E, 49cm; wdlc-5, 48°46′31.19″ N, 126°8′19.61″ E, 43cm ) using gravity corer in June 2009, respectively. Both cores were sectioned at an interval of 1.0cm.LOI550℃ (loss on ignition) , total phosphorus ( TP), total nitrogen ( TN ) , susceptibilitie, grain size distribution and elements were analyzed to construct environmental changes of Wudalianchi Lake. Sediment chronology was established based on the highest 137Cs activity peak ( 1963A. D. ) , the first ^137Cs activity appearance ( 1952A. D. ) and ^210Pb data. The average sediment rate is 0.28g/cm^2· a or 0.59cm/a, and 0.25g/cm^2· a or 0.55cm/a for the wdlc-3 and wdlc-5 cores in the past century. Combined with the sediment age, environmental changes of Wudalianehi Lake were reconstructed. The results showed that the environmental history could be divided into four stages as follows: 1920s- 1950s, median diameter of sediments was large, TN and LOI550℃ showed increased trends, Al and Fe contents of core sediment also increased,which indieats that lake environmental changes were possibly related with human activity such as land reclamation. 1950s - 1980s, human activity (such as deforestation, destruction of grassland) became the main influences which led to TN, Al and Fe contents to increase. However, median diameter was small. 1980s - 2000s, total nitrogen and phosphorus increased more rapidly, heavy metals also showed an increase trend, which could be attributed to extensive use of fertilizers, pesticides, phosphorus-containing items, leaded gasoline,and development of industry. Since 2000s,eutrophication has been the most import

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期刊信息
  • 《第四纪研究》
  • 中国科技核心期刊
  • 主管单位:中国科学院
  • 主办单位:中国科学院地质与地球物理研究所 中国第四纪研究委员会
  • 主编:郭正堂
  • 地址:北京9825信箱
  • 邮编:100029
  • 邮箱:dsj@mail.igcas.ac.cn dsjs@mail.igcas.ac.cn
  • 电话:010-82998119
  • 国际标准刊号:ISSN:1001-7410
  • 国内统一刊号:ISSN:11-2708/P
  • 邮发代号:82-428
  • 获奖情况:
  • 1996年被国务院学位委员会地球物理及地质学科评议...,2001年入中国期刊方阵,2007年获中国科学院出版基金科技期刊排行榜三等奖
  • 国内外数据库收录:
  • 美国化学文摘(网络版),英国动物学记录,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:17826