Arid
DOI10.1016/j.geomorph.2006.10.007
A field investigation into the effects of progressive rainfall-induced soil seal and crust development on runoff and erosion rates: The impact of surface cover
Neave, Mel1; Rayburg, Scott2
通讯作者Neave, Mel
来源期刊GEOMORPHOLOGY
ISSN0169-555X
出版年2007
卷号87期号:4页码:378-390
英文摘要

Surface crusts and seals can form from a variety of processes, both physical and biological, and have the potential to alter runoff and erosion, especially in regions with low vegetation covers. Despite the obvious links between seals and crusts these features have rarely been considered together. This study uses rainfall simulation experiments to investigate interrill soil crust and seal development in response to structural (or raindrop-impact-induced) and depositional (or runoff-induced) processes on a semiarid piedmont in southern New Mexico, USA, which has undergone substantive vegetation change (replacement of grasses by shrubs) over the last 100 years. The study design incorporates six double-paired runoff plots divided into four subplots, each of which was exposed to three rainfall simulation events. Crust development on these plots was assessed using penetration-resistance measurements while seal development was assessed using runoff coefficients. The penetration-resistance data indicate that subplots directly exposed to raindrop impacts (uncovered plots) have crusts that are similar to 40% stronger than those positioned beneath a mesh cover (covered plots) that intercepts the kinetic energy of the rainfall. The crusts exposed to raindrop-impacts increased in strength following each simulation, whereas the crusts on the covered surfaces reached a plateau after two events.


Runoff data indicate that seal development does not directly mirror crust formation. Runoff coefficients increased after each rainfall simulation event but were not significantly different between the covered and uncovered plots. Rather, the presence of stone lags or litter on the soil surface influenced the relation between runoff and seal development. Sediment yields from uncovered surfaces exceeded those from covered surfaces, indicating that raindrop impacts contribute to the delivery of sediment into flows. The results of this study indicate that the loss of vegetation cover on the piedmont has increased the extent of surface crust and seal development but that those crusts may be playing an important role in mitigating erosion. (c) 2006 Elsevier B.V. All rights reserved.


英文关键词rainfall simulation structural crust depositional crust semiarid vegetation change infiltration
类型Article
语种英语
国家Australia
收录类别SCI-E
WOS记录号WOS:000251894700010
WOS关键词SOUTHERN NEW-MEXICO ; SHRUBLAND ECOSYSTEMS ; CHIHUAHUAN DESERT ; WATER ; GRASSLAND ; INFILTRATION
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向Physical Geography ; Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/154340
作者单位1.Univ Sydney, Sch Geosci, Div Geog, Sydney, NSW 2006, Australia;
2.Univ Canberra, Water Res Lab, Canberra, ACT 2601, Australia
推荐引用方式
GB/T 7714
Neave, Mel,Rayburg, Scott. A field investigation into the effects of progressive rainfall-induced soil seal and crust development on runoff and erosion rates: The impact of surface cover[J],2007,87(4):378-390.
APA Neave, Mel,&Rayburg, Scott.(2007).A field investigation into the effects of progressive rainfall-induced soil seal and crust development on runoff and erosion rates: The impact of surface cover.GEOMORPHOLOGY,87(4),378-390.
MLA Neave, Mel,et al."A field investigation into the effects of progressive rainfall-induced soil seal and crust development on runoff and erosion rates: The impact of surface cover".GEOMORPHOLOGY 87.4(2007):378-390.
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