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DatoValore
TitleHYPROP-FIT to Model Rock Water Retention Curves Estimated by Different Methods
AbstractThe water retention curve, which relates the matric potential, y, to the water content, q, is essential to describe the flow processes in the unsaturated zone and provides useful information for environmental and engineering applications. There are few studies devoted to measuring the rock water retention curves due to the rock's tightness, which makes it more technically difficult to use specific methods. In this study, we tested four different methods to measure water retention curves of two lithotypes of carbonate porous rocks with the aim to find the most effective to be applied to rock samples. Suction table, evaporation, Quasi-Steady Centrifuge, and WP4-T dewpoint potentiameter methods have been applied. The Quasi-Steady Centrifuge method proved to be the only one capable of determining water retention curves in the entire water content range and capturing the bimodality of the tested media with respect to the other methods. The measured water retention data were fitted with HYPROP-FIT software that allows us to accurately describe the WRCs and obtain critical parameters for the numerical simulation of flow and transport through the vadose zone, which plays a key role in various environmental issues.
SourceWater (Basel) 14
Keywordsunsaturated carbonate rockQuasi-Steady Centrifuge methodWP4-T dewpoint potentiameterevaporation methodsuction table methodbimodal hydraulic functions
JournalWater (Basel)
EditorMolecular Diversity Preservation International, Basel,
Year2022
TypeArticolo in rivista
DOI10.3390/w14213443
AuthorsMaria Clementina Caputo, Lorenzo De Carlo, Antonietta Celeste Turturro
Text488879 2022 10.3390/w14213443 unsaturated carbonate rock Quasi Steady Centrifuge method WP4 T dewpoint potentiameter evaporation method suction table method bimodal hydraulic functions HYPROP FIT to Model Rock Water Retention Curves Estimated by Different Methods Maria Clementina Caputo, Lorenzo De Carlo, Antonietta Celeste Turturro CNR National Research Council, IRSA Water Research Institute, Via Francesco De Blasio 5, 70132 Bari, Italy; CNR National Research Council, IRSA Water Research Institute, Via Francesco De Blasio 5, 70132 Bari, Italy; CNR National Research Council, IRSA Water Research Institute, Via Francesco De Blasio 5, 70132 Bari, Italy The water retention curve, which relates the matric potential, y, to the water content, q, is essential to describe the flow processes in the unsaturated zone and provides useful information for environmental and engineering applications. There are few studies devoted to measuring the rock water retention curves due to the rock s tightness, which makes it more technically difficult to use specific methods. In this study, we tested four different methods to measure water retention curves of two lithotypes of carbonate porous rocks with the aim to find the most effective to be applied to rock samples. Suction table, evaporation, Quasi Steady Centrifuge, and WP4 T dewpoint potentiameter methods have been applied. The Quasi Steady Centrifuge method proved to be the only one capable of determining water retention curves in the entire water content range and capturing the bimodality of the tested media with respect to the other methods. The measured water retention data were fitted with HYPROP FIT software that allows us to accurately describe the WRCs and obtain critical parameters for the numerical simulation of flow and transport through the vadose zone, which plays a key role in various environmental issues. 14 Published version https //www.mdpi.com/2073 4441/14/21/3443 23/10/2022 Articolo in rivista Molecular Diversity Preservation International 2073 4441 Water Basel Water Basel Water Basel Water. Basel antoniettacelesteturturro TURTURRO ANTONIETTA CELESTE mariaclementina.caputo CAPUTO MARIA CLEMENTINA lorenzo.decarlo DE CARLO LORENZO