2 results

Steady infiltration rate: Relation to antecedent soil moisture, soil permeability, and measurement method and period

Lucas Raimundo Rauber ORCID logo , Dalvan José Reinert ORCID logo , Paulo Ivonir Gubiani ORCID logo , Suelen Matiasso Fachi ORCID logo

16/Jan/2024

ABSTRACT Soil steady water infiltration rate (SIR) is a key variable in hydrological modeling, but its relationship to antecedent soil moisture is not yet well understood. We tested the hypothesis that the SIR decreases with the increase in antecedent moisture, and that this relationship depends on permeability to water on the soil surface, the measurement method, and the measurement period. We conducted an experiment in an Argissolo Vermelho-Amarelo Distrófico abrúptico (Psammentic Paleudult – Soil Taxonomy), measuring infiltration in up to […]

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Rock-soil skeleton increases water infiltration

Suélen Matiasso Fachi ORCID logo , Paulo Ivonir Gubiani ORCID logo , Fabrício de Araújo Pedron ORCID logo , Lucas Raimundo Rauber ORCID logo

28/Nov/2023

ABSTRACT A widespread assumption among researchers and technicians is that stony soils are more susceptible to degradation. However, the role of rock fragments in the hydrology of stony soils, especially in regard to infiltration, is still a research gap. The aim of this study was to test the hypothesis that an increase in rock fragments in the soil profile increases the water infiltration rate. Infiltration tests using a double-ring infiltrometer were conducted on February 11, 2021, and December 11, 2022, […]

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