印度喜马偕尔邦两个湖芯的沉积学和粒度特征

IF 0.7 Q4 METEOROLOGY & ATMOSPHERIC SCIENCES
Neha Kholia, B. Kotlia, D. Porinchu, Kamini Bisht, Anupam Sharma, Poonam Jalal
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引用次数: 0

摘要

利用印度喜马偕尔邦(Himachal Pradesh)的Khajjiar湖(长746 cm)和Rewalsar湖(长647 cm)的两个湖泊岩心,了解其沉积学特征和粒度分布的变化。两个湖心年龄均为全新世上。Rewalsar湖沉积物以粉砂为主,含少量粘土,而Khajjiar湖沉积物含砂、粉砂和粘土,两种岩心均含高碳质物质。Khajjiar湖的标准偏差为0.88 ~ 2.56 φ, Rewalsar湖的标准偏差为0.957 ~ 2.264 φ,表明岩心沉积物分选差至极差。Khajjiar湖的峰度值在0.678 ~ 1.205 φ之间,Rewalsar湖的峰度值在0.8 ~ 1.2.4 φ之间,呈平峰形到细峰形。Khajjiar湖的偏度值为-0.097 ~ 0.240 φ, Rewalsar湖的偏度值为0.079 ~ 0.25 φ,呈现出精细到对称的偏度模型。利用粒度参数对二元图进行了解释。卡贾尔湖沉积物总有机碳(TOC)含量较高,为0.9 ~ 31.2%;平均值为10.6%),而Rewalsar湖沉积物的平均值为1.0 ~ 9.0;av。2.6%)。沉积学特征表明,能量条件与该地区普遍存在的气候条件有关。总体而言,卡贾尔湖岩心沉积物相对较粗,受干旱条件影响较大,而雷瓦尔萨尔湖岩心则受较低能量条件的影响。Khajjiar湖表现为波动条件(第1区)到湿润条件(第2区)再到干旱条件(第3区)的转变,Rewalsar湖表现为波动条件(第1区)到湿润条件(第2区和第3区)的转变。两湖剖面1区和2区的相似性表明,两湖在沉积过程中经历了相似的气候条件,表明波动和干旱条件占主导地位。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Sedimentological and Grain Size Characteristics of Two Lake Cores from Himachal Pradesh, India
Two lake cores from Khajjiar (length 746 cm) and Rewalsar lakes (length 647 cm) in Himachal Pradesh (India) were retrieved to understand the sedimentological characteristics and variation in grain size distribution. Both the lake cores are Upper Holocene in age. The Rewalsar lake sediments are composed predominantly of silt with small amounts of clay, whereas the Khajjiar sediments contain sand, silt and clay and both cores have high carbonaceous matter. The standard deviation ranges from 0.88 ϕ to 2.56 ϕ for Khajjiar lake and from 0.957 ϕ to 2.264 ϕ for Rewalsar lake, indicating poorly to very poorly sorted core sediments. The values of the Kurtosis vary between 0.678 ϕ and 1.205 ϕ for Khajjiar lake and from 0.8 ϕ to 1.2.4 ϕ for Rewalsar lake, viewing platykurtic to leptokurtic nature. Further, the skewness value ranges from -0.097 ϕ to 0.240 ϕ for Khajjiar lake and 0.079 ϕ to 0.25 ϕ for Rewalsar lake revealing fine to symmetrical skewness model. The bivariate plots by using the grain-size parameters were also interpreted. The Total Organic Carbon (TOC) is higher in the Khajjiar lake sediments (0.9 to 31.2%; av. 10.6%), compared to that in the Rewalsar lake sediments (1.0 to 9.0; av. 2.6%). The sedimentological characteristics indicate that the energy conditions were linked to the climatic conditions prevailing in the area. In general, the Khajjiar lake core is composed of relatively coarser sediments and more affected by arid conditions while the fine fraction of the Rewalsar shows the consequence of lower energy conditions. The Khajjiar lake shows the transition from fluctuating conditions (zone 1) to humid (zone 2) to arid (zone 3), while the Rewalsar shows the change from fluctuating (zone 1) to humid conditions (zones 2 and 3). The similarity between zone 1 and 2 of both the lake profiles shows that both lakes have experienced similar climatic conditions during the deposition, revealing domination of fluctuating and arid conditions.
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来源期刊
Journal of Climate Change
Journal of Climate Change METEOROLOGY & ATMOSPHERIC SCIENCES-
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16.70%
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