Interpreting and simulating hydrological processes need a large number of field saturated soil hydraulic conductivity, K-fs, data that should be collected with simple and rapid field experiments. A Simplified method based on a Beerkan Infiltration run (SBI method) was recently developed and tested successfully on Burundian soils. With the SBI method, a cylinder is inserted to a short depth into the soil and the infiltration time of a few small volumes of water repeatedly applied at the surface of the confined soil is measured. Calculating K-fs needs the slope of the linearized cumulative infiltration vs. time relationship and an estimate of the so called alpha* parameter. In this investigation, the SBI method was validated with reference to a larger dataset, also including different Sicilian soils. The alpha* value of first approximation (0.012 mm(-1)) yielded an estimate of K-fs differing in general by not more than a factor of three from the K-fs values obtained by the more complete and onerous BEST (Beerkan Estimation of Soil Transfer parameters) procedure of soil hydraulic characterization. The K-fs values obtained with SBI method were also very close (means differing by a factor of 1.01) to the ones determined with the One Ponding Depth relationship for the single ring pressure infiltrometer technique. Detection of physically plausible relationships between alpha* and the slope of the linearized infiltration curve indicated that the measured infiltration process contains the necessary information to estimate alpha*. Different alpha* predictive relationships for Sicily and Burundi allowed to obtain estimates of K-fs never differing by more than a factor of three from the corresponding values obtained with BEST. The developed method is a good candidate method for intensively sampling an area of interest. Points needing developments include tests with other datasets, comparisons with independent measurements of both alpha* and K-fs, and maybe development of an improved experimental methodology to obtain the infiltration data. (C) 2013 The Authors. Published by Elsevier B.V.

Testing a Simplified Approach to Determine Field Saturated Soil Hydraulic Conductivity / Bagarello, V.; Castellini, M.; Di Prima, S.; Giordano, G.; Iovino, M.. - In: PROCEDIA ENVIRONMENTAL SCIENCES. - ISSN 1878-0296. - 19:(2013), pp. 599-608. [10.1016/j.proenv.2013.06.068]

Testing a Simplified Approach to Determine Field Saturated Soil Hydraulic Conductivity

Bagarello, V.
;
Di Prima, S.;Iovino, M.
2013-01-01

Abstract

Interpreting and simulating hydrological processes need a large number of field saturated soil hydraulic conductivity, K-fs, data that should be collected with simple and rapid field experiments. A Simplified method based on a Beerkan Infiltration run (SBI method) was recently developed and tested successfully on Burundian soils. With the SBI method, a cylinder is inserted to a short depth into the soil and the infiltration time of a few small volumes of water repeatedly applied at the surface of the confined soil is measured. Calculating K-fs needs the slope of the linearized cumulative infiltration vs. time relationship and an estimate of the so called alpha* parameter. In this investigation, the SBI method was validated with reference to a larger dataset, also including different Sicilian soils. The alpha* value of first approximation (0.012 mm(-1)) yielded an estimate of K-fs differing in general by not more than a factor of three from the K-fs values obtained by the more complete and onerous BEST (Beerkan Estimation of Soil Transfer parameters) procedure of soil hydraulic characterization. The K-fs values obtained with SBI method were also very close (means differing by a factor of 1.01) to the ones determined with the One Ponding Depth relationship for the single ring pressure infiltrometer technique. Detection of physically plausible relationships between alpha* and the slope of the linearized infiltration curve indicated that the measured infiltration process contains the necessary information to estimate alpha*. Different alpha* predictive relationships for Sicily and Burundi allowed to obtain estimates of K-fs never differing by more than a factor of three from the corresponding values obtained with BEST. The developed method is a good candidate method for intensively sampling an area of interest. Points needing developments include tests with other datasets, comparisons with independent measurements of both alpha* and K-fs, and maybe development of an improved experimental methodology to obtain the infiltration data. (C) 2013 The Authors. Published by Elsevier B.V.
2013
Inglese
Four Decades of Progress in Monitoring and Modeling of Processes in the Soil-Plant- Atmosphere System: Applications and Challenges
Contributo
19
599
608
10
ELSEVIER SCIENCE BV
SARA BURGERHARTSTRAAT 25, PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
Internazionale
Soil hydraulic properties; Measurement methods; BEST (Beerkan Estimation of Soil Transfer parameters) procedure; Single ring pressure infiltrometer
Testing a Simplified Approach to Determine Field Saturated Soil Hydraulic Conductivity / Bagarello, V.; Castellini, M.; Di Prima, S.; Giordano, G.; Iovino, M.. - In: PROCEDIA ENVIRONMENTAL SCIENCES. - ISSN 1878-0296. - 19:(2013), pp. 599-608. [10.1016/j.proenv.2013.06.068]
4 Contributo in Atti di Convegno (Proceeding)::4.1 Contributo in Atti di convegno
Bagarello, V.; Castellini, M.; Di Prima, S.; Giordano, G.; Iovino, M.
273
5
none
info:eu-repo/semantics/conferenceObject
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11388/228449
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