A Technical Note: Orientation of Cracks and Hydrology in a Shrink-Swell Soil

Abstract

Crack orientations are an important soil physical property that affects water flow, particularly in vertic soils. However, the spatial and temporal variability of crack orientations across different land uses and gilgai features is not welldocumented and addressed in hydrology models. Thus; there is a need to quantify crack orientations for different land uses and to incorporate their spatial and temporal dynamics into hydrological models. Our objectives were to document the spatial variability of cracks orientations across two land uses and to demonstrate the potential importance of crack orientation related to the hydrology of Vertisols. The exploratory field measurements of the spatial distribution of crack orientations across two Vertisol catenae of two land uses and gilgai features are presented. The field survey showed the complexity of crack geometry in a field, the potential impact of crack orientation on Vertisol hydrology and the challenges associated with measurement of crack orientations.

Enhancing Furrow Irrigation Performance and Water Productivity Through Better Design and Water Management in a Cracked Soil

“…Management of water resources in Vertisols is more problematic compared to other soil groups. When the soils of this group dry, cracks are formed and these cracks facilitate rapid transport of surface water into the subsoil through preferential flow (6). Jafari (15) evaluated the irrigation management in a silty clay paddy soil using three levels of crack width and three depths of irrigation water to refill cracks.…”