Abstract
Saturated hydraulic conductivity (Ks) is a quantitative measure of saturated soil properties and it is essential for designing irrigation, drainage and waste water systems, modelling studies for understanding and prediting rates of infiltration, runoff, erosion, seepage, upflux, solute transport and migration of pollutant to groundwater. However, the accuracy of Ks is highly dependent on the method used, soil and surface characteristics. The objective of the study was to compare Ks methods such as two in situ [Double ring infiltrometer (DRI), air entry permeameter (AEP)] and one pedotransfer function (PTF) based methods for four different land uses such as paddy field (PADF), mango field (MANF), cashew field (CASF) and playground (PLAG). The Ks obtained from the DRI, AEP and PTF methods were used to study the effect of the method and land use on Ks and suitability of a method for a land use. It was observed that the measured Ks data using AEP and DRI of different land uses follow a log-normal distribution. The mean Ks were significantly different for both measuring technique and the land use. The AEP resulted highest (2.64 mm/h) and PTF lowest (1.59 mm/h) values of Ks, respectively for all land uses, whereas the Ks was highest (2.47 mm/h) and lowest (1.75 mm/h) for the land uses CASF and PLAG, respectively. For all land uses, the mean Ks were highest for AEP followed by DRI, and PTF methods. The order of Ks obtained for the land uses were CASF (2.51 mm/h), MANF (1.87 mm/h), PADF (1.82 mm/h) and PLAG (1.71 mm/h). Spatial variability of Ks was observed for DRI method and the land use PLAG. The selection of best suitable method for a particular situation can be obtained by optimizing the interdependent parameters, including method to be used, accuracy in instrument and measurement methods, soil condition and the numbers of practical constraints of the investigation (e.g., cost, availability of manpower, time requirement, portability of estimate, simplicity in measuring technique, operating condition).
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References
Reynolds, W.D.: Saturated hydraulic conductivity: Laboratory measurement. In: Carter, M.R. (ed.) Soil Sampling and Methods of Analysis, pp. 589–598 (1993)
Shukla, M., Lal, R.: Transport of dissolve organic carbon through soil columns. Annual Meeting of ASA/SSSA Seattle, WA, p. 31 (2004)
Prieksat, M.A., Kaspar, T.C., Ankeny, M.D.: Positional and temporal changes in pounded infiltration in corn field. Soil Sci. Soc. Am. J. 58, 181–184 (1994)
Lekamalage, W.B.: Characterization of surface soil hydraulic conductivity in sloping landscapes. Thesis Submitted to the College of Graduate Studies and Research in Partial Fulfillment of the Requirements for the Degree of Master of Science in the Department of Soil Science University of Saskatchewan Saskatoon, pp. 1–4 (2003)
Lee, H.J.: Comparing the inverse parameter estimation approach with pedo-transfer function method for estimating soil hydraulic conductivity. Geosci. J. 9(3), 269–276 (2005)
Kechavarzi, C., Dawson, Q., Leeds-Harrison, P.B.: Physical properties of low-lying agricultural peat soils in England. Geoderma 154, 196–202 (2010)
Jarvis, N., Koestel, J., Messing, I., Moeys, J., Lindahl, A.: influence of soil, land use and climatic factors on the hydraulic conductivity of soil. Hydrol. Earth Syst. Sci. 17, 5185–5195 (2013)
Holden, J., Burt, T.P.: Hydraulic conductivity in upland blanket peat. Measur. Var. Hydrological Process. 17, 1227–1237 (2003)
Rossiter, G.D., Jatten, G.V.: Effects of soil depth and saturated hydraulic conductivity spatial variation on runoff simulation by Limburg soil erosion model (LISEM). A Case Study in Faucon Catchment, France. Enschede, the Nederland’s (2011)
Nielsen, D.R., Biggar, J.W., Erh, K.T.: Spatial variability of field-measured soil-water properties. Hilgardia 42, 215–259 (1973)
Darzi, A., Yari, A., Bagheri, H., Sabe, G., Yari, R.: Study of variation of saturated hydraulic conductivity with time. J. Irrig. Drain. Eng. 134, 479–484 (2008)
Bagarello, V., Provenzano, G., Sgroi, A.: Fitting particle size distribution models to data from burundian soils for the best procedure and other purposes. Biosys. Eng. 4, 435–441 (2009)
Dev, K.S., Shukla, K.M.: Variability of hydraulic conductivity due to multiple factors. Am. J. Environ. Sci. 8(5), 489–502 (2012)
Reynolds, D.W., Bowman, B.T., Brunke, R.R., Drury, C.F., Tan, C.S.: Comparison of tension infiltrometer, pressure infiltrometer, and soil core estimates of saturated hydraulic conductivity. Soil Sci. Soc. Am. J. 64, 478–484 (2000)
Bagarello, B., Castellini, M., Di Prima, S., Giordano, G., Iovino, M.: Testing a simplified approach to determine field saturated soil hydraulic conductivity. Procedia Environ. Sci. 19, 599–608 (2013)
Klute, A.: Laboratory measurement of hydraulic conductivity of saturated soil. In: Black, C.A. (ed.). Methods of Soil Analysis, Part 1, pp. 210–221 (1965)
Lee, M.D., Reynolds, D.W., Elrick, E.D., Clotheier, E.B.: A comparison of three field method for measuring saturated hydraulic conductivity. Can. J. Soil Sci. 65, 563–573 (1985)
Klute, A., Dirksen, C.: Hydraulic conductivity and diffusivity: laboratory methods. In: Methods of Soil Analysis: Part 1—Physical and Mineralogical Methods, pp. 687–734 (1986)
Grant, C.D., Groenevelt, P.H.: Weighting the differential water capacity to account for declining hydraulic conductivity in a drying coarse-textured soil. Soil Res. 53(4), 386–391 (2015)
Jačka, L., Pavlásek, J., Kuráž, V., Pech, P.: A comparison of three measuring methods for estimating the saturated hydraulic conductivity in the shallow subsurface layer of mountain podzols. Geoderma 219, 82–88 (2014)
Burgy, R.H., Luthin, J.N.: A test of the single and double ring type infiltrometers. Trans. Am. Geophys. Union 37, 189–191 (1956)
Bagarello, V., Iovino, M., Lai, J.B.: Field and numerical tests of the two-ponding depth procedure for analysis of single-ring pressure infiltrometer data. Pedosphere 23(6), 779–789 (2013)
Elrick, D.E., Reynolds, W.D., Tan, K.A.: Hydraulic conductivity measurements in the unsaturated zone using improved well analyses. Groundw. Monit. Remediat. 9(3), 184–193 (1989)
Bouwer, H.: A double tube method for measuring hydraulic conductivity of soil in situ above a water table. In: Soil Science Society of America Proceedings, vol. 25, pp. 334–342 (1961)
Perroux, K.M., White, I.: Designs for disc permeameters. Soil Sci. Soc. Am. J. 52, 1205–1215 (1988)
Bouwer, H.: Rapid field measurement of air entry value and hydraulic conductivity of soil as significant parameters in flow system analysis. Water Resour. Res. 2, 729–738 (1966)
Bagarello, V., Iovino, M., Elrick, D.: A simplified falling-head technique for rapid determination of field saturated hydraulic conductivity. Soil Sci. Soc. Am. J. 68, 66–73 (2004)
Topp, G.C., Binns, M.N.: Field measurement of hydraulic conductivity with a modified air entry permeameter. Can. J. Soil Sci. 56, 139–147 (1976)
Mohanty, B.P., Kanwar, S.R., Everts, J.C.: Comparison of saturated hydraulic conductivity measurement methods for a glacial-till soil. soil Sci. Soc. Am. J. 58(3), 672–677 (1994)
Bodhinayake, W., Si, C.B.: Near-saturated surface soil hydraulic properties under different land uses in the St Denis National Wildlife Area, Saskatchewan, Canada. Hydrol. Process. 18, 2835–2850 (2004)
Fallico, C., Migliari, E., Troisi, S.: Comparison of three measurement methods of saturated hydraulic conductivity. Hydrol. Earth Syst. Sci. Discuss. 3, 987–1019 (2006)
Bagarello, V., Sgroi, A.: Using the single-ring infiltrometer method to detect temporal changes in surface soil field saturated hydraulic conductivity. Soil Tillage Res. 76(1), 13–24 (2004)
Fodor, N., Sandor, R., Orfanus, T., Lichne, L., Rajkai, K.: Evaluation method dependency of measured saturated hydraulic conductivity. Geoderma 165, 60–68 (2011)
Ronayne, M.J., Houghton, T.B., Stednick, J.D.: Field characterization of hydraulic conductivity in a heterogeneous alpine glacial till. J. Hydrol. Eng. 458(459), 103–109 (2012)
Runbin, D.R., Fedler, B.C., Borrelli, J.: Comparison of methods to estimate saturated hydraulic conductivity in texas soils with grass. J. Irrig. Drain. Eng. 138(4), 322–327 (2012)
Bagarello, V., Baiamonte, G., Castellini, M., Di Prima, D., Iovino, M.: A comparison between the single ring pressure infiltrometer and simplified falling head techniques. Hydrol. Process. 28, 4843–4853 (2014)
Hall, D.G., Reeve, M.J., Thomasson, A.J., Wright, A.F.: Water Retention, Porosity and Density of Field Soils. Soil Survey of England and Wales. Rothamsted Experimental Station, Harpenden, UK (1977)
Campbell, G.S.: Soil Physics with Basic: Transport Models for Soil Plant Systems. Elsevier Science, New York (1985)
Rawls, W.J., Gimenez, D., Grossman, R.: Use of soil texture, bulk density and slope of the water retention curve to predict saturated hydraulic conductivity. Am. Soc. Agric. Biol. Eng. 41(4), 983–988 (1998)
Smettem, K.R.J., Bristow, K.L.: Obtaining soil hydraulic properties for water balance and leaching models from survey data. 2. Hydraulic conductivity. Aust. J. Agric. Res. 50(7), 1259–1262 (1999)
Wösten, J.H.M., Pachepsky, Y.A., Rawls, W.J.: Pedotransfer functions: bridging the gap between available basic soil data and missing soil hydraulic characteristics. J. Hydrol. 251, 123–150 (2001)
Wosten, J.H.M., Lilly, A., Nemes, A., Le Bas, C.: Development and use of a database of hydraulic properties of European soils. Geoderma 90, 169–185 (1999)
Schaap, M.G., Leij, F.J., Van Genuchten, M.T.: Rosetta: A computer program for estimating soil hydraulic parameters with hierarchical pedotransfer functions. J. Hydrol. 251, 163–176 (2001)
Wagner, B., Tarnawski, V.R., Hennings, V., Müller, U., Wessolek, G., Plagge, R.: Evaluation of pedo-transfer functions for unsaturated soil hydraulic conductivity using an independent data set. Geoderma 102, 275–297 (2001)
Bouma, J.: Measuring the hydraulic conductivity of soil horizons with continuous macropores. Soil Sci. Soc. Am. J. 46, 438–441 (1983)
Nielsen, D.R., Wendroth, O.: Spatial and Temporal Statistics—Sampling Field Soils and Their Vegetation. Catena, Reiskirchen, Germany, p. 416 (2003)
Bormann, H., Klaassen, K.: Seasonal and land use dependent variability of soil hydraulic and soil hydrological properties of two northern german soils. Geoderma 145, 295–302 (2008)
Hu, W., Shao, M., Wang, Q., She, D.: Effects of measurement method, scale, and landscape features on variability of saturated hydraulic conductivity. J. Hydrol. Eng. 18, 378–386 (2013)
Reynolds, W.D., Elrick, D.E., Young, E.G.: Ring or cylinder infiltrometers (vadose zone). In: Dane, J.H., Topp, G.C. (eds.) Methods of Soil Analysis, Part 4: Physical Methods. Soil Science Society of America Journal Madison, pp. 818–843 (2002)
Hu, W., Shao, M., Wang, Q., Fan, J., Horton, R.: Temporal changes of soil hydraulic properties under different land uses. Geoderma 149(3–4), 355–366 (2009)
Carter, M.R., Gregorich, E.G.: Soil Sampling and Methods of analysis. Canadian Society of Soil Science, Pinawa, Manitoba (2008)
Rao, M.D., Raghuwanshi, N.S., Singh, R.: Development of a physically based 1d-infiltration model for irrigated soils. Agric. Water Manag. 85(1), 165–174 (2006)
Nimmo, J.R., Schmidt, K.M., Perkins, K.S., Stock, J.D.: Rapid measurement of field-saturated hydraulic conductivity for areal characterization. Vadose Zone J. 8(1), 142–149 (2009)
Schaap, M.G.: Rosetta Version 1.0. U.S. Salinity Laboratory, ARS, U.S. Department of Agriculture, Riverside, CA. (1999)
Alvarez-Acosta, C., Lascano, R.J., Stroosnijder, L.: Test of the Rosetta pedotransfer function for saturated hydraulic conductivity. Open J. Soil Sci. 2(3), 203–212 (2012)
Schaap, M.G., Van Genuchten, M.T.: A modified Mualem-Van Genuchten formulation. Vadose Zone J. 5, 27–34 (2006)
Aldabagh, A.S.Y., Beer, C.E.: Field measurement of hydraulic conductivity above a water table with air-entry permeameter. Am. Soc. Agric. Biol. Eng. 14(1), 29–31 (1971)
Nemati, M.R., Caron, J., Banton, O., Tardif, P.: Determining air entry value in peat substrates. Soil Sci. Soc. Am. J. 66(2), 367–373 (2002)
Van Den Berg, J.A., Louters, T.: The variability of soil moisture diffusivity of loamy to silty soils on marl, determined by the hot air method. J. Hydrol. 97(3), 235–250 (1988)
Chapuis, R.P.: Predicting the saturated hydraulic conductivity of sand and gravel using effective diameter and void ratio. Can. Geotech. J. 41(5), 787–795 (2004)
Park, E., Smucker, A.: Saturated hydraulic conductivity and porosity within macro aggregates modified by tillage. Soil Sci. Soc. Am. J. 69(1), 38–45 (2005)
Zhou, X., Lin, H.S., White, E.A.: Surface soil hydraulic properties in four soil series under different land uses and their temporal changes. CATENA 73(2), 18–188 (2008)
Matthews, G.P., Laudone, G.M., Gregory, A.S., Bird, N.R.A., Matthews, A.G., Whalley, W.R.: Measurement and simulation of the effect of compaction on the pore structure and saturated hydraulic conductivity of grassland and arable soil. Water Resour. Res. 10.1029/2009WR007720 (2010)
Zhang, X.C., Norton, L.D.: Effect of exchangeable mg on saturated hydraulic conductivity disaggregation and clay dispersion of disturbed soils. J. Hydrol. 260(1–4), 194–205 (2002)
Lado, M., Paz, A., Ben-Hur, M.: Organic matter and aggregate size interactions in saturated hydraulic conductivity. Soil Sci. Soc. Am. J. 68(1), 234–242 (2004)
Dusa, A.A.: Effect of bulk density on saturated hydraulic conductivity. J. Eng. Appl. Sci. 5(1), 159–165 (2013)
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Islam, A., Mailapalli, D.R., Behera, A. (2019). Comparison of Saturated Hydraulic Conductivity Methods for Sandy Loam Soil with Different Land Uses. In: Rathinasamy, M., Chandramouli, S., Phanindra, K., Mahesh, U. (eds) Water Resources and Environmental Engineering I. Springer, Singapore. https://doi.org/10.1007/978-981-13-2044-6_10
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