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Soil Pore Network Complexity Changes Induced by Wetting and Drying Cycles—A Study Using X-ray Microtomography and 3D Multifractal Analyses

Dados Bibliográficos

ID15479250
AutoresJocenei A T de Oliveira (0000-0001-9830-8027, Universidade Estadual de Ponta Grossa), Fabio Augusto Meira Cássaro (0000-0002-7240-3947, Universidade Estadual de Ponta Grossa), Adolfo Posadas (0000-0001-5378-1064), Adolfo N D Posadas (AgriEntech Ltda, São Carlos 13560-460, SP, Brazil), Luiz F Pires (0000-0001-5073-5900, Universidade Estadual de Ponta Grossa, autor correspondente)
Ano2022
Volume19
Fascículo17
Páginas10582-10582
Data de publicação2022-08-25
Open AccessSim
TipoARTICLE
PeriódicoInternational Journal of Environmental Research and Public Health (JOURNAL)
Identificadores do periódicoISSN: 1661-7827 • E-ISSN: 1660-4601
EditoraMultidisciplinary Digital Publishing Institute (PUBLISHER • CH)
DOI10.3390/ijerph191710582
PMID36078295
OpenAlexW4293104053
IdiomaEN
Referências citadas60

Soils are dynamic and complex systems in their natural state, which are subjected to profound changes due to management. Additionally, agricultural soils are continuously exposed to wetting and drying (W-D) cycles, which can cause modifications in the complexity of their pores. Thus, we explore how successive W-D cycles can affect the pore network of an Oxisol under contrasting managements (conventional tillage-CT, minimum tillage-MT, no tillage-NT, and secondary forest-F). The complexity of the soil pore architecture was evaluated using a 3D multifractal approach combined with lacunarity, Shannon's entropy, and pore geometric parameters. Our results showed that the multifractal approach effectively identified and quantified the changes produced in the soil pore architecture by the W-D cycles. The lacunarity curves revealed important aspects of the modifications generated by these cycles. Samples under F, NT, and MT suffered the most significant changes. Pore connectivity and tortuosity were largely affected by the cycles in F and NT. Our findings demonstrated that the 3D geometric parameters and normalized Shannon's entropy are complementary types of analysis. According to the adopted management, they allowed us to separate the soil into two groups according to their similarities (F and NT; CT and MT)

Agronomy · Composite material · Fractal · Fractal dimension · Lacunarity · Mineralogy · Multifractal system · Porosity · Soil water · Tillage · Wetting · Environmental Science · Landslides and related hazards · Materials Science · Mathematics · Soil and Unsaturated Flow · Soil Geostatistics and Mapping · Geology · Soil Science

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