Surface Crusting
Surface Crusting is a soil structural degradation process characterized by the formation of a thin, dense, low-permeability layer at the soil surface due to the dispersion and downward migration of fine particles under the influence of rainfall or irrigation impact, commonly occurring in sodic soils.
165
Publications
8.4K
Citations
436
Authors
210
Institutions
Publications per year
2017–2026
22
Variants
Soil Crusting
Parents
165
SOIL SPLASH AND THE FORMATION OF SURFACE CRUSTS BY RAINDROP IMPACT
DS McIntyre · Soil Science · 1958 · 262 citations
1–5 of 165
436
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6
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Laboratoire Interuniversitaire des Systèmes Atmosphériques, France
3 publications · 313 citations
3
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3
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3
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1–5 of 436
210
Soil Science Research Unit
Orléans, France
9 h-index
22 publications
1.6K citations
Institute of Soil and Water Conservation
Yangling, China
5 h-index
7 publications
172 citations
Institut de Recherche pour le Développement
Marseille, France
5 h-index
8 publications
517 citations
Northwest A&F University
Yangling, China
4 h-index
10 publications
261 citations
Institut National de la Recherche Agronomique
Rabat, Morocco
4 h-index
13 publications
628 citations

Centre National de la Recherche Scientifique
Paris, France
4 h-index
10 publications
766 citations
Laboratoire Interuniversitaire des Systèmes Atmosphériques
Créteil, France
3 h-index
6 publications
805 citations
Hebrew University of Jerusalem
Jerusalem, Israel
3 h-index
6 publications
480 citations
1–8 of 210
SSSAJ · 15 publications · 1K citations
14
h-index
8 publications · 623 citations
8
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8 publications · 486 citations
8
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8 publications · 818 citations
8
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7 publications · 424 citations
7
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