Soil–Water–Atmosphere Effects on Soil Crack Characteristics under Field Conditions in a Semiarid Climate

Soil’s physical and hydrological properties influence the proper modeling, planning, and management of water resources and soil conservation. In areas of vertic soils subjected to wetting and drying cycles, the soil–water–atmosphere interaction is complex and understudied at the field scale, especia...

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Main Authors: Jacques Carvalho Ribeiro Filho, Eunice Maia de Andrade, Maria Simas Guerreiro, Helba Araújo de Queiroz Palácio, José Bandeira Brasil
Format: Article
Language:English
Published: MDPI AG 2023-04-01
Series:Hydrology
Subjects:
Online Access:https://www.mdpi.com/2306-5338/10/4/83
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author Jacques Carvalho Ribeiro Filho
Eunice Maia de Andrade
Maria Simas Guerreiro
Helba Araújo de Queiroz Palácio
José Bandeira Brasil
author_facet Jacques Carvalho Ribeiro Filho
Eunice Maia de Andrade
Maria Simas Guerreiro
Helba Araújo de Queiroz Palácio
José Bandeira Brasil
author_sort Jacques Carvalho Ribeiro Filho
collection DOAJ
description Soil’s physical and hydrological properties influence the proper modeling, planning, and management of water resources and soil conservation. In areas of vertic soils subjected to wetting and drying cycles, the soil–water–atmosphere interaction is complex and understudied at the field scale, especially in dry tropical regions. This work quantifies and analyzes crack development under field conditions in an expansive soil in a semiarid region for both the dry and rainy seasons. Six 1 m<sup>2</sup> plots in an experimental 2.8 ha watershed were photographed and direct measurements were taken of the soil moisture and crack area, depth and volume once a week and after a rainfall event from July 2019 to June 2020. The rainfall was monitored for the entire period and showed a unimodal distribution from December to May after five months without precipitation. The cracks were first sealed in the plots with a predominance of sand and when the soil moisture was above 23% and had an accumulated precipitation of 102 mm. The other plots sealed their cracks when the soil moisture was above 32% and with an accumulated precipitation in the rainy season above 222 mm. The cracks redeveloped after sealing upon a reduction of 4% in the soil moisture. The depth of the cracks showed a better response to climatic variations (total precipitation, soil moisture and continuous dry and wet days). The higher clay content and the higher plasticity index plots developed more cracks with greater depth and volume.
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spelling doaj.art-4204a395822445d39a0f8a6512011ebe2023-11-17T19:30:18ZengMDPI AGHydrology2306-53382023-04-011048310.3390/hydrology10040083Soil–Water–Atmosphere Effects on Soil Crack Characteristics under Field Conditions in a Semiarid ClimateJacques Carvalho Ribeiro Filho0Eunice Maia de Andrade1Maria Simas Guerreiro2Helba Araújo de Queiroz Palácio3José Bandeira Brasil4Departamento de Engenharia Agrícola, Campus do Pici, Universidade Federal do Ceará, Fortaleza CEP 60455-760, BrazilDepartamento de Conservação de Solo e Água, Universidade Federal Rural do Semi-Arido, Rua Francisco Mota, 572, Mossoró CEP 59625-900, BrazilI3ID, Universidade Fernando Pessoa, Praça 9 de Abril, 349, 4249-004 Porto, PortugalInstituto Federal de Educação, Ciência e Tecnologia do Ceará, Rodovia Iguatu-Várzea Alegre km, 5, Iguatu CEP 63503-790, BrazilDepartamento de Engenharia Agrícola, Campus do Pici, Universidade Federal do Ceará, Fortaleza CEP 60455-760, BrazilSoil’s physical and hydrological properties influence the proper modeling, planning, and management of water resources and soil conservation. In areas of vertic soils subjected to wetting and drying cycles, the soil–water–atmosphere interaction is complex and understudied at the field scale, especially in dry tropical regions. This work quantifies and analyzes crack development under field conditions in an expansive soil in a semiarid region for both the dry and rainy seasons. Six 1 m<sup>2</sup> plots in an experimental 2.8 ha watershed were photographed and direct measurements were taken of the soil moisture and crack area, depth and volume once a week and after a rainfall event from July 2019 to June 2020. The rainfall was monitored for the entire period and showed a unimodal distribution from December to May after five months without precipitation. The cracks were first sealed in the plots with a predominance of sand and when the soil moisture was above 23% and had an accumulated precipitation of 102 mm. The other plots sealed their cracks when the soil moisture was above 32% and with an accumulated precipitation in the rainy season above 222 mm. The cracks redeveloped after sealing upon a reduction of 4% in the soil moisture. The depth of the cracks showed a better response to climatic variations (total precipitation, soil moisture and continuous dry and wet days). The higher clay content and the higher plasticity index plots developed more cracks with greater depth and volume.https://www.mdpi.com/2306-5338/10/4/83vertic soilscrack dynamicstropical dry regionssemiarid
spellingShingle Jacques Carvalho Ribeiro Filho
Eunice Maia de Andrade
Maria Simas Guerreiro
Helba Araújo de Queiroz Palácio
José Bandeira Brasil
Soil–Water–Atmosphere Effects on Soil Crack Characteristics under Field Conditions in a Semiarid Climate
Hydrology
vertic soils
crack dynamics
tropical dry regions
semiarid
title Soil–Water–Atmosphere Effects on Soil Crack Characteristics under Field Conditions in a Semiarid Climate
title_full Soil–Water–Atmosphere Effects on Soil Crack Characteristics under Field Conditions in a Semiarid Climate
title_fullStr Soil–Water–Atmosphere Effects on Soil Crack Characteristics under Field Conditions in a Semiarid Climate
title_full_unstemmed Soil–Water–Atmosphere Effects on Soil Crack Characteristics under Field Conditions in a Semiarid Climate
title_short Soil–Water–Atmosphere Effects on Soil Crack Characteristics under Field Conditions in a Semiarid Climate
title_sort soil water atmosphere effects on soil crack characteristics under field conditions in a semiarid climate
topic vertic soils
crack dynamics
tropical dry regions
semiarid
url https://www.mdpi.com/2306-5338/10/4/83
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