TY - JOUR
T1 - Spatial distribution of surface properties, runoff generation and landscape development in the Zin Valley Badlands, northern Negev, Israel
AU - Kuhn, Nikolaus J.
AU - Yair, Aaron
AU - Grubin, Milica Kasanin
PY - 2004/10
Y1 - 2004/10
N2 - Infiltration tests, soil mapping and soil property analysis were used to assess the effect of within-storm rainfall conditions on spatial patterns of surface characteristics relevant for runoff generation, continuity and erosion in the Zin Valley Badlands. Runoff and erosion differ strongly between ridges and slopes. Soils at both locations are susceptible to sealing, but on the sideslopes deep desiccation cracks inhibit continuous flow, even during high magnitude rainstorms. The discontinuous nature of runoff has a feedback on surface conditions. Erosion on the ridges maintains shallow soils prone to sealing while infiltration and deposition on the sideslopes enhance soil depth, a prerequisite for stable desiccation cracks. Some runoff generated on the ridges is transmitted to the valley via rills. On straight sideslopes, rills are single and often discontinuous, indicating limited frequency of continuous runoff. Along concave valley heads, rill systems are well integrated and continuous, concentrating runoff and reducing infiltration losses along slopes. The longitudinal, V-shaped valley morphology of small catchments in the Zin Valley Badlands reflects the long-term effect of different erosion rates in valley heads and on sideslopes. Over time, valley incision lengthened the sideslopes, reducing the portion of annual rainfall that was runoff-effective. Once sideslopes reached a critical length that inhibited frequent continuous flow, a colluvium with an increased infiltration capacity developed, reducing runoff frequency even further. Consequently, erosion on the valley sideslopes decreased. Continuous flow from ridges to the valley channel remained more common in integrated rill systems in concavities and valley heads, leading to more erosion and retreat of the valley heads. The spatial patterns of runoff and erosion in the Zin Valley Badlands demonstrate that landscape development is strongly affected by processes that lead to differentiation of soil properties on hillslopes with uniform lithology. The patterns of surface characteristics and their role in landscape development are strongly dependent on rainfall conditions, highlighting the need for geomorphologists to identify the dynamic spatial and temporal scales relevant for landscape development.
AB - Infiltration tests, soil mapping and soil property analysis were used to assess the effect of within-storm rainfall conditions on spatial patterns of surface characteristics relevant for runoff generation, continuity and erosion in the Zin Valley Badlands. Runoff and erosion differ strongly between ridges and slopes. Soils at both locations are susceptible to sealing, but on the sideslopes deep desiccation cracks inhibit continuous flow, even during high magnitude rainstorms. The discontinuous nature of runoff has a feedback on surface conditions. Erosion on the ridges maintains shallow soils prone to sealing while infiltration and deposition on the sideslopes enhance soil depth, a prerequisite for stable desiccation cracks. Some runoff generated on the ridges is transmitted to the valley via rills. On straight sideslopes, rills are single and often discontinuous, indicating limited frequency of continuous runoff. Along concave valley heads, rill systems are well integrated and continuous, concentrating runoff and reducing infiltration losses along slopes. The longitudinal, V-shaped valley morphology of small catchments in the Zin Valley Badlands reflects the long-term effect of different erosion rates in valley heads and on sideslopes. Over time, valley incision lengthened the sideslopes, reducing the portion of annual rainfall that was runoff-effective. Once sideslopes reached a critical length that inhibited frequent continuous flow, a colluvium with an increased infiltration capacity developed, reducing runoff frequency even further. Consequently, erosion on the valley sideslopes decreased. Continuous flow from ridges to the valley channel remained more common in integrated rill systems in concavities and valley heads, leading to more erosion and retreat of the valley heads. The spatial patterns of runoff and erosion in the Zin Valley Badlands demonstrate that landscape development is strongly affected by processes that lead to differentiation of soil properties on hillslopes with uniform lithology. The patterns of surface characteristics and their role in landscape development are strongly dependent on rainfall conditions, highlighting the need for geomorphologists to identify the dynamic spatial and temporal scales relevant for landscape development.
KW - Badlands
KW - Landscape development
KW - Partial area contribution
KW - Rainfall characteristics
KW - Soil properties
UR - http://www.scopus.com/inward/record.url?scp=7244257602&partnerID=8YFLogxK
U2 - 10.1002/esp.1115
DO - 10.1002/esp.1115
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AN - SCOPUS:7244257602
SN - 0197-9337
VL - 29
SP - 1417
EP - 1430
JO - Earth Surface Processes and Landforms
JF - Earth Surface Processes and Landforms
IS - 11
ER -