Accounting for Calcareous Concretions in Calcic Vertisols Improves the Accuracy of Soil Hydraulic Property Estimations
- 16 November 2017
- journal article
- research article
- Published by Wiley in Soil Science Society of America Journal
- Vol. 81 (6) , 1296-1302
Abstract
Core Ideas: Calcareous concretions (CCs) could maintain a considerable amount of water and the water content of CCs decreased with an increase in CC sizes. The addition of CCs to soils changed the WRC and the pore distribution of soils significantly. The available water content (AWC) of soil–CC mixtures decreased when the CC content increased. A linear equation, which included CC content and CC water content, was proposed to estimate the AWC of soils containing CCs accurately. The soil water retention curve (WRC) is one of the most important properties in soil hydraulic studies. Current studies normally focus on fine soils, ignoring the water‐holding capacity of coarse fragments (>2 mm) and their effects on soil available water content (AWC). Calcareous concretions (CC) are coarse inclusions distributed widely in soils around the world. This study was conducted to quantify the effects of the proportion and size of CCs on the soil WRC and AWC of a calcic vertisol. The WRCs of CCs were measured using the sand box and ceramic plate method, and the WRCs of fine soils and soil–CC mixtures of various sizes (2–5, 5–8, and 8–30) and proportions (5, 10, 15, and 30% on a total mass basis) of CC were determined with the centrifuge method. The WRCs were fitted with the van Genuchten equation. The results showed that CCs retained a considerable amount of water. The saturated water contents of CCs of 2‐ to 5‐, 5‐ to 8‐ and 8‐ to 30‐mm were 0.251, 0.220, and 0.196 cm 3 cm –3 , respectively. The addition of CCs changed the WRC and pore distribution of soils significantly. The AWC of soil–CC mixtures decreased with increasing CC content. A linear equation, which included the fraction of CCs and water content in CCs, was proposed to estimate the AWC of soils containing CCs accurately. Accounting for CCs in the calcic vertisol improved the accuracy of soil hydraulic property estimations.Keywords
Funding Information
- the national key Research and Development Program of China (2016YFD0300801)
- the National Key Technology R&D Program of China (2012BAD05B00)
This publication has 33 references indexed in Scilit:
- Modeling the Soil Water Retention Curves of Soil-Gravel Mixtures with Regression Method on the Loess Plateau of ChinaPLOS ONE, 2013
- Soil water characteristic curve measurement without bulk density changes and its implications in the estimation of soil hydraulic propertiesGeoderma, 2011
- Validation of an analytical method for determining soil hydraulic properties of stony soils using experimental dataGeoderma, 2010
- The water retention of a granite rock fragments in High Tatras stony soilsJournal of Hydrology and Hydromechanics, 2010
- Influence of rock fragments on the water retention and water percolation in a calcareous soilCATENA, 2003
- Moisture Characteristics of Hanford Gravels: Bulk, Grain‐Surface, and Intragranular ComponentsVadose Zone Journal, 2003
- Relationships between shrinkage indices and soil properties in some New Zealand soilsGeoderma, 2002
- Water Holding Capacity of Ironstone Gravel in a Typic Plinthoxeralf in Southeast AustraliaSoil Science Society of America Journal, 2000
- Sample size for determination of coarse fragment content in a stony soilGeoderma, 1994
- Rock fragments in top soils: significance and processesCATENA, 1994