干旱区地理 ›› 2021, Vol. 44 ›› Issue (5): 1317-1327.doi: 10.12118/j.issn.1000–6060.2021.05.13
贺振杰1,2,3(),马龙1,2,3(),吉力力·阿不都外力1,2,3,刘文1,2,3,Gulnura ISSANOVA2,4,Galymzhan SAPAROV2,5,黄坤1,2,3
收稿日期:
2020-06-13
修回日期:
2021-01-27
出版日期:
2021-09-25
发布日期:
2021-09-22
通讯作者:
马龙
作者简介:
贺振杰(1995-),男,硕士研究生,主要从事湖泊沉积与环境演变研究. E-mail: 基金资助:
HE Zhenjie1,2,3(),MA Long1,2,3(),Jilili ABUDUWAILI1,2,3,LIU Wen1,2,3,Gulnura ISSANOVA2,4,Galymzhan SAPAROV2,5,HUANG Kun1,2,3
Received:
2020-06-13
Revised:
2021-01-27
Online:
2021-09-25
Published:
2021-09-22
Contact:
Long MA
摘要:
湖泊沉积物中的粒度参数记载了丰富的流域环境变化信息,可为无器测资料地区重建古环境变化序列提供可靠的途径。通过对巴尔喀什湖岩芯沉积物中粒度、磁化率等环境代用指标的分析,结合放射性137Cs定年以及流域气候、湖泊水位等器测记录数据,研究了巴尔喀什湖沉积物中粒度变化特征及其环境指示意义。结果表明:巴尔喀什湖沉积物中黏土质(<4 μm)组分平均含量为20.32%,细粉砂质(4~16 μm)为40.13%,中粉砂质(16~32 μm)为22.86%,粗粉砂质(32~64 μm)为10.55%,砂质(>64 μm)为6.13%。通过粒径标准-偏差法提取了沉积物中环境细颗粒敏感组分(F1,6.61~10.00 μm)和粗颗粒敏感组分(F2,45.71~69.18 μm)。研究表明在人类活动影响不断加强的背景下,粒度敏感组分的含量变化不能敏感的反映湖泊水位、入湖径流乃至区域气候的变化,而与沉积物中磁化率所反映的人类活动强度变化存在较为显著的相关关系(r=0.870,P<0.01),这可能与人类活动增强导致的流域内富含磁性物质的细颗粒碎屑物质被搬运入湖有关,湖泊沉积物中磁化率升高的同时,湖泊沉积物中细颗粒物质增加。研究结果可为长时间尺度下古环境重建研究提供重要参考依据,同时也对揭示流域人类活动对湖泊环境的影响具有一定的科学意义。
贺振杰,马龙,吉力力·阿不都外力,刘文,Gulnura ISSANOVA,Galymzhan SAPAROV,黄坤. 哈萨克斯坦巴尔喀什湖沉积物粒度特征及其对区域环境变化的响应[J]. 干旱区地理, 2021, 44(5): 1317-1327.
HE Zhenjie,MA Long,Jilili ABUDUWAILI,LIU Wen,Gulnura ISSANOVA,Galymzhan SAPAROV,HUANG Kun. Grain-size characteristics of lacustrine sediments in Balkhash Lake, Kazakhstan and its response to regional environmental changes[J]. Arid Land Geography, 2021, 44(5): 1317-1327.
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