Runoff and erosion processes and rates in the Zin valley badlands, northern Negev, Israel.

A. Yair; H. Lavee; R. B. Bryan; E. Adar

doi:10.1002/esp.3760050301

Runoff and erosion processes and rates in the Zin valley badlands, northern Negev, Israel.

A. Yair
, H. Lavee
, R. B. Bryan
, E. Adar

Department of Geography

Research output: Contribution to journal › Article › peer-review

89 Scopus citations

Abstract

Experiments show that due to the high stability and strong flocculation of clay-rich aggregates rainsplash is ineffective in surface sealing so that infiltration capacities remain high despite intense, prolonged rainfall. North-facing slopes respond more quickly, more frequently and produce more runoff than south-facing slopes. Present-day surface flow must be extremely infrequent and denudation rates very low. -from Authors

Original language	English
Pages (from-to)	205-225
Number of pages	21
Journal	Earth Surface Processes and Landforms
Volume	5
Issue number	3
DOIs	https://doi.org/10.1002/esp.3760050301
State	Published - 1980

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10.1002/esp.3760050301

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title = "Runoff and erosion processes and rates in the Zin valley badlands, northern Negev, Israel.",

abstract = "Experiments show that due to the high stability and strong flocculation of clay-rich aggregates rainsplash is ineffective in surface sealing so that infiltration capacities remain high despite intense, prolonged rainfall. North-facing slopes respond more quickly, more frequently and produce more runoff than south-facing slopes. Present-day surface flow must be extremely infrequent and denudation rates very low. -from Authors",

author = "A. Yair and H. Lavee and Bryan, \{R. B.\} and E. Adar",

year = "1980",

doi = "10.1002/esp.3760050301",

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AU - Yair, A.

AU - Lavee, H.

AU - Bryan, R. B.

AU - Adar, E.

PY - 1980

Y1 - 1980

N2 - Experiments show that due to the high stability and strong flocculation of clay-rich aggregates rainsplash is ineffective in surface sealing so that infiltration capacities remain high despite intense, prolonged rainfall. North-facing slopes respond more quickly, more frequently and produce more runoff than south-facing slopes. Present-day surface flow must be extremely infrequent and denudation rates very low. -from Authors

AB - Experiments show that due to the high stability and strong flocculation of clay-rich aggregates rainsplash is ineffective in surface sealing so that infiltration capacities remain high despite intense, prolonged rainfall. North-facing slopes respond more quickly, more frequently and produce more runoff than south-facing slopes. Present-day surface flow must be extremely infrequent and denudation rates very low. -from Authors

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AN - SCOPUS:0018907754

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JO - Earth Surface Processes and Landforms

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ER -

Runoff and erosion processes and rates in the Zin valley badlands, northern Negev, Israel.

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