Impacts of geographic variability and geologic history on the distribution of post-settlement alluvium (PSA) across the upper Midwest, USA

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Alison M. Anders , Bruce L. Rhoads
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引用次数: 0

Abstract

Accelerated floodplain sedimentation related to agricultural development of uplands has produced post-settlement alluvium (PSA) along rivers throughout the upper Midwest, U.S.A. Landscape characteristics, surficial sediments, and soils in the region vary geographically in relation to differences in geologic history, yet the extent to which this geographic variability influences PSA accumulation remains unexplored. This study uses existing data to assess how non-dimensional PSA thickness varies with landscape characteristics, surficial sediments, soils and climate. Geographic variability is associated with three subregions: 1) areas glaciated during the Late Wisconsin Episode (LWE), 2) areas glaciated during Pre-Illinois and Illinois Episodes (PI&IE), and 3) the Paleozoic Plateau (PP), an area where evidence of Quaternary glaciation is highly localized and does not influence geomorphic characteristics of the landscape. These subregions differ significantly in average geomorphic characteristics, including mean watershed slope (WS), mean local relief (LR), fraction of non-contributing area (NCA), pre-settlement drainage density (DD), and mean normalized river steepness (KSN). Native vegetation type also differs systematically between the subregions, creating significant differences in the frequency of alfisols (Alfi) and molisols (Mol). Thickness of last glacial loess (Loess) also varies across the region, although not systematically between the subregions identified. Non-dimensional PSA thickness differs significantly among the subregions, increasing systematically with landscape age, reflecting faster upland erosion rates and stronger connectivity of uplands to river corridors in older landscapes relative to more recently glaciated landscapes. Non-dimensional PSA thickness is significantly positively correlated with LR, KSN, WS, Loess, Alfi, and Mol and significantly negatively correlated with NCA. Non-visibly distinct PSA is present in some LWE watersheds characterized by significantly lower KSN and WS relative to other LWE watersheds in which PSA is visibly distinct. PSA thickness and visibility reflect catchment-wide landscape characteristics and watershed-scale river steepness, which emphasize the importance of geographic setting, geological history, and landscape geomorphic characteristics for understanding historical river sediment dynamics. Spatial variability in PSA thickness also serves as an indicator of river system sensitivity to land-use change, providing insight into the relative impact of humans on rivers within different geographic settings.
地理变异和地质历史对美国上中西部沉降后冲积层(PSA)分布的影响
与高地农业开发相关的河漫滩加速沉积在美国中西部上游河流沿线产生了沉降后冲积层(PSA)。该地区的景观特征、地表沉积物和土壤因地质历史的差异而在地理上有所不同,但这种地理变异性对PSA积累的影响程度仍未得到探索。本研究使用现有数据来评估无量纲PSA厚度如何随景观特征、地表沉积物、土壤和气候而变化。地理变率与三个次区域有关:1)晚期威斯康辛时期(LWE)的冰川区,2)前伊利诺斯州和伊利诺斯州时期(PI&;IE)的冰川区,以及3)古生代高原(PP),第四纪冰川作用的证据高度局限,不影响景观的地貌特征。这些分区在平均流域坡度(WS)、平均局部坡度(LR)、非贡献面积比例(NCA)、沉降前排水密度(DD)和平均标准化河流陡度(KSN)等平均地貌特征上存在显著差异。原生植被类型在各亚区之间也存在系统差异,造成了溶解石(Alfi)和溶解石(Mol)出现频率的显著差异。末次冰期黄土(黄土)的厚度在整个区域内也有变化,尽管在确定的次区域之间没有系统的变化。各子区域间无量纲PSA厚度差异显著,随景观年龄的增加而系统增加,反映出相对于最近的冰川景观,较老景观的高地侵蚀速度更快,高地与河流廊道的连通性更强。无因次PSA厚度与LR、KSN、WS、黄土、Alfi、Mol呈显著正相关,与NCA呈显著负相关。与PSA明显不同的其他LWE流域相比,一些以KSN和WS显著降低为特征的LWE流域存在不明显的PSA。PSA的厚度和可见度反映了流域范围的景观特征和流域尺度的河流陡度,这强调了地理环境、地质历史和景观地貌特征对理解历史河流泥沙动力学的重要性。PSA厚度的空间变异性还可以作为河流系统对土地利用变化敏感性的指标,从而深入了解不同地理环境下人类对河流的相对影响。
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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