采用定量原产地分析 (QPA) 方法量化马格达莱纳河上游(哥伦比亚)沉积物生成和沉积通量的控制因素:1.自然和人为对泥沙组分的控制

IF 3.5 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
S. Liedel, L. Caracciolo, J. C. Restrepo, G. J. Weltje, F. Lucà, A. Beltrán-Triviño, J. D. Restrepo Ángel
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引用次数: 0

摘要

本研究调查了马格达莱纳河上游流域(哥伦比亚),该流域的特点是构造活动、热带气候、异质岩性组合和人类影响。研究旨在通过将 27 个近期河道样本的岩相学数据与地球化学、地貌参数、历史降水量、土地覆盖、滑坡和悬浮沉积物负荷数据相结合,了解控制沉积物生成、通量和组成的因素。分析表明,沙粒成分与排水岩性分布不匹配。研究提出了一套新的末段混合模型,量化了侵蚀性、沙土生成潜力(与岩性有关)以及山坡与河流出口之间的沉积物连通性(与地貌有关)的影响。结果表明,由于侵蚀性高,沉积岩的沉积物生成量增加(最多达 40%),而由于形态参数的控制,中低品位变质岩的沉积物流量减少(最多达 60%)。由于矿物学和纹理参数的控制,板岩和高品位变质岩所占比例过高,而火山岩所占比例过低(高达 100%)。在火山活动地区,山体滑坡活动的增强偶尔会掩盖由形态和岩性特征驱动的全流域成分趋势,因为它控制着砂粒中火山岩和低品位变质岩碎屑的罕见高比例。水电站大坝截留的沉积物使悬浮沉积物通量大幅减少了 30%,而森林砍伐对沉积物通量的影响很小。这项研究强调了在任何以沉积物生成为重点的研究中,将沉积物生成、地貌和与地震活动有关的随机事件分布结合起来的重要性,以及在定量产状分析(QPA)中开发数值模型的重要性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

A Quantitative Provenance Analysis (QPA) Approach to Quantify Controls on Sediment Generation and Sediment Flux in the Upper Reaches of the Magdalena River (Colombia): 1. Natural and Anthropic Controls on the Sand Fraction

A Quantitative Provenance Analysis (QPA) Approach to Quantify Controls on Sediment Generation and Sediment Flux in the Upper Reaches of the Magdalena River (Colombia): 1. Natural and Anthropic Controls on the Sand Fraction

This study investigates the upper Magdalena river basin (Colombia), which is characterized by tectonic activity, tropical climate, heterogeneous lithological assemblages, and anthropic influence. It aims to comprehend factors controlling sediment generation, flux, and composition by incorporating petrographic data from 27 recent fluvial samples along with geochemistry, geomorphological parameters, historical precipitation, land cover, landsliding and suspended sediment load data. The analysis shows mismatches between sand composition and drainage lithology distribution. A new set of endmember mixing models is presented, quantifying the impacts of erodibility, sand generation potential (related to lithology), and sediment connectivity between hillslopes and river outlets (related to geomorphology). Results show enhanced sediment generation from sedimentary rocks (up to 40%) due to high erodibility, and decreased sediment flux from low- to medium-grade metamorphic rocks (up to 60%) due to controlling morphometric parameters. Overrepresentation of plutonic and high-grade metamorphic rocks and underrepresentation of volcanic rocks (up to 100%) are controlled by mineralogical and textural parameters. Enhanced landsliding activity in areas with volcanic activity occasionally overshadows basin-wide compositional trends driven by morphological and lithological characteristics, as it controls rare overrepresentation of volcanic and low-grade metamorphic detritus in the sand fraction. Sediment retention by hydroelectric dams significantly decreases suspended sediment flux by 30%, while deforestation plays a minor role in sediment flux. This study underscores the importance of coupling sediment generation, geomorphology and the distribution of stochastic events related to seismic activity in any sediment production-focused study and for developing numerical models in Quantitative Provenance Analysis (QPA).

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来源期刊
Journal of Geophysical Research: Earth Surface
Journal of Geophysical Research: Earth Surface Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
6.30
自引率
10.30%
发文量
162
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