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RESEARCH ARTICLE

Size of subsoil clods affects soil-water availability in sand–clay mixtures

Giacomo Betti A , Cameron D. Grant A B , Robert S. Murray A and G. Jock Churchman A
+ Author Affiliations
- Author Affiliations

A University of Adelaide, School of Agriculture, Food & Wine, Waite Campus PMB 1, Glen Osmond, SA 5064, Australia.

B Corresponding author. Email: cameron.grant@adelaide.edu.au

Soil Research 54(3) 276-290 https://doi.org/10.1071/SR15115
Submitted: 22 April 2015  Accepted: 18 July 2015   Published: 11 April 2016

Abstract

Clay delving in strongly texture-contrast soils brings up subsoil clay in clumps ranging from large clods to tiny aggregates depending on the equipment used and the extent of secondary cultivation. Clay delving usually increases crop yields but not universally; this has generated questions about best management practices. It was postulated that the size distribution of the subsoil clumps created by delving might influence soil-water availability (and hence crop yield) because, although the clay increases water retention in the root-zone, it can also cause poor soil aeration, high soil strength and greatly reduced hydraulic conductivity. We prepared laboratory mixtures of sand and clay-rich subsoil in amounts considered practical (10% and 20% by weight) and excessive (40% and 60% by weight) with different subsoil clod sizes (<2, 6, 20 and 45 mm), for which we measured water retention, soil resistance, and saturated hydraulic conductivity. We calculated soil water availability by traditional means (plant-available water, PAW) and by the integral water capacity (IWC). We found that PAW increased with subsoil clay, particularly when smaller aggregates were used (≤6 mm). However, when the potential restrictions on PAW were taken into account, the benefits of adding clay reached a peak at ~40%, beyond which IWC declined towards that of pure subsoil clay. Furthermore, the smaller the aggregates the less effective they were at increasing IWC, particularly in the practical range of application rates (<20% by weight). We conclude that excessive post-delving cultivation may not be warranted and may explain some of the variability found in crop yields after delving.

Additional keywords: aggregate size distribution, soil physical limitation, sandy soils, tillage.


References

Asgarzadeh H, Mosaddeghi M, Mahboubi A, Nosrati A, Dexter AR (2010) Soil water availability for plants as quantified by conventional available water, least limiting water range and integral water capacity. Plant and Soil 335, 229–244.
Soil water availability for plants as quantified by conventional available water, least limiting water range and integral water capacity.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BC3cXhtFOrt73P&md5=592c581c1c965b32d0927f55f53dd02eCAS |

Bailey G, Hughes B, Tonkin R, Dowie R, Watkins N (2010) Gross soil modification of duplex soils through delving and spading. In ‘19th World Congress of Soil Science’. Brisbane. (International Union of Soil Sciences) Available at: http://iuss.org/19th%20WCSS/Symposium/pdf/0773.pdf

Betti G, Grant C, Churchman G, Murray R (2015) Increased profile wettability in texture-contrast soils from clay delving: case studies in South Australia. Soil Research 53, 125–136.
Increased profile wettability in texture-contrast soils from clay delving: case studies in South Australia.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BC2MXjvVOltbo%3D&md5=2de593d76f4cd5daf4b4f623b0d2c910CAS |

Brown KW, Evans GB, Thomas JC (1985) Increased soil water retention by mixing horizons of shallow sandy soils. Soil Science 139, 118–121.
Increased soil water retention by mixing horizons of shallow sandy soils.Crossref | GoogleScholarGoogle Scholar |

Cann MA (2000) Clay spreading on water repellent sands in the south east of South Australia—promoting sustainable agriculture. Journal of Hydrology 231–232, 333–341.
Clay spreading on water repellent sands in the south east of South Australia—promoting sustainable agriculture.Crossref | GoogleScholarGoogle Scholar |

Cockroft B, Olsson KA (2000) Degradation of soil structure due to coalescence of aggregates in no-till, no-traffic beds in irrigated crops. Australian Journal of Soil Research 38, 61–70.
Degradation of soil structure due to coalescence of aggregates in no-till, no-traffic beds in irrigated crops.Crossref | GoogleScholarGoogle Scholar |

Cockroft B, Barley KP, Greacen EL (1969) The penetration of clays by fine probes and root tips. Australian Journal of Soil Research 7, 333–348.
The penetration of clays by fine probes and root tips.Crossref | GoogleScholarGoogle Scholar |

Costa A, Albuquerque JA, da Costa A, Pértile P, da Silva FR (2013) Water retention and availability in soils of the State of Santa Catarina-Brazil: effect of textural classes, soil classes and lithology. Revista Brasileira de Ciencia do Solo 37, 1535–1548.
Water retention and availability in soils of the State of Santa Catarina-Brazil: effect of textural classes, soil classes and lithology.Crossref | GoogleScholarGoogle Scholar |

da Silva AP, Kay BD, Perfect E (1994) Characterisation of the least limiting water range of soils. Soil Science Society of America Journal 58, 1775–1781.
Characterisation of the least limiting water range of soils.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DyaK2MXitlCjsLw%3D&md5=992364d8fbfc4d66c6a638a33ed7c42fCAS |

Davenport D, Hughes B, Davies S, Hall D, and Rural Solution SA Agricultural Bureau of South Australia, Caring for our Country, Grains Research Development Corporation (2011) ‘Spread, delve, spade, invert: A best practice guide to the addition of clay to sandy soils.’ (Grains Research and Development Corporation: Kingston, ACT)

Desbiolles JMA, Fielke JM, Chaplin P (1997) An application of tine configuration to obtain subsoil delving for the management of non-wetting sands. In ‘3rd International Conference on Soil Dynamics (ICSD III)’. Tiberias, Israel. pp. 201–210. (Faculty of Agricultural Engineering, Technion—Israel Institute of Technology: Haifa, Israel)

Eldridge R (2007) Clay delving at Parilla. University of Adelaide Crop Science Newsletter Archive. Available at: www.adelaide.edu.au/css/newsletters/archive/2000s/Eldridge_delving_2007.pdf

Fernández-Gálvez J, Barahona E (2005) Changes in soil water retention due to soil kneading. Agricultural Water Management 76, 53–61.
Changes in soil water retention due to soil kneading.Crossref | GoogleScholarGoogle Scholar |

Gardner WR (1958) Some steady-state solutions of the unsaturated moisture flow equation with application to evaporation from a water table. Soil Science 85, 228–232.
Some steady-state solutions of the unsaturated moisture flow equation with application to evaporation from a water table.Crossref | GoogleScholarGoogle Scholar |

Gardner WK, Fawcett RG, Steed GR, Pratley JE, Whitfield DM, Van RH (1992) Crop production on duplex soils in south-eastern Australia. Australian Journal of Experimental Agriculture 32, 915–927.
Crop production on duplex soils in south-eastern Australia.Crossref | GoogleScholarGoogle Scholar |

Gill JS, Tisdall J, Sukartono, Kusnarta IGM, McKenzie BM (2004) Physical properties of a clay loam soil mixed with sand. In ‘SuperSoil 2004: 3rd Australian & New Zealand Soils Conference’. 5–9 December 2004. (The Regional Institute Ltd: Gosford, NSW) Available at: www.regional.org.au/au/asssi/supersoil2004/s14/poster/1585_gillj.htm

Grant CD, Groenevelt PH (2015) Weighting the differential water capacity to account for declining hydraulic conductivity in a drying coarse-textured soil. Soil Research 53, 386–391.
Weighting the differential water capacity to account for declining hydraulic conductivity in a drying coarse-textured soil.Crossref | GoogleScholarGoogle Scholar |

Grant CD, Groenevelt PH, Robinson NI (2010) Application of the Groenevelt–Grant soil water retention model to predict the hydraulic conductivity. Soil Research 48, 447–458.
Application of the Groenevelt–Grant soil water retention model to predict the hydraulic conductivity.Crossref | GoogleScholarGoogle Scholar |

Groenevelt PH, Grant CD, Semetsa S (2001) A new procedure to determine soil water availability. Australian Journal of Soil Research 39, 577–598.
A new procedure to determine soil water availability.Crossref | GoogleScholarGoogle Scholar |

Hall D, Lemon J, Oliver Y, Gazey C, Davies S, Russell C, Witham N (2009) Managing south coast sandplain soils to yield potential. Bulletin No. 4773, October 2009. Department of Agriculture and Food, Western Australia. Albany, W. Aust.

Hall DJM, Jones HR, Crabtree WL, Daniels TL (2010) Claying and deep ripping can increase crop yields and profits on water repellent sands with marginal fertility in southern Western Australia. Australian Journal of Soil Research 48, 178–187.
Claying and deep ripping can increase crop yields and profits on water repellent sands with marginal fertility in southern Western Australia.Crossref | GoogleScholarGoogle Scholar |

Hamblin A, Richards Q, Blake J (1988) Crop growth across a toposequence controlled by depth of sand over clay. Australian Journal of Soil Research 26, 623–635.
Crop growth across a toposequence controlled by depth of sand over clay.Crossref | GoogleScholarGoogle Scholar |

Hardie MA, Cotching WE, Doyle RB, Holz G, Lisson S, Mattern K (2011) Effect of antecedent soil moisture on preferential flow in a texture-contrast soil. Journal of Hydrology 398, 191–201.
Effect of antecedent soil moisture on preferential flow in a texture-contrast soil.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BC3MXhslGgtb8%3D&md5=df9f98477d0170d2eab7eafbd27a18e5CAS |

Harper RJ, Gilkes RJ (2004) The effects of clay and sand additions on the strength of sandy topsoils. Australian Journal of Soil Research 42, 39–44.
The effects of clay and sand additions on the strength of sandy topsoils.Crossref | GoogleScholarGoogle Scholar |

Harper RJ, McKissock I, Gilkes RJ, Carter DJ, Blackwell PS (2000) A multivariate framework for interpreting the effects of soil properties, soil management and landuse on water repellency. Journal of Hydrology 231–232, 371–383.
A multivariate framework for interpreting the effects of soil properties, soil management and landuse on water repellency.Crossref | GoogleScholarGoogle Scholar |

Isbell R (2002) ‘The Australian Soil Classification.’ Revised edn. (CSIRO Publishing: Melbourne)

Kramer PJ (1949) ‘Plant and soil water relationships.’ (McGraw Hill Book Co.: New York)

Lipiec J, Walczak R, Witkowska-Walczak B, Nosalewicz A, Slowinska-Jurkiewicz A, Slawinski C (2007) The effect of aggregate size on water retention and pore structure of two silt loam soils of different genesis. Soil & Tillage Research 97, 239–246.
The effect of aggregate size on water retention and pore structure of two silt loam soils of different genesis.Crossref | GoogleScholarGoogle Scholar |

MacGillivray JH, Doneen LD (1942) Soil moisture conditions as related to the irrigation of truck crops on mineral soils. Proceedings American Society for Horticultural Science 40, 483–492.

Marshall TJ, Holmes JW, Rose CW (1996) ‘Soil physics.’ (Cambridge University Press: Cambridge, UK)

Martínez E, Fuentes J-P, Silva P, Valle S, Acevedo E (2008) Soil physical properties and wheat root growth as affected by no-tillage and conventional tillage systems in a Mediterranean environment of Chile. Soil & Tillage Research 99, 232–244.
Soil physical properties and wheat root growth as affected by no-tillage and conventional tillage systems in a Mediterranean environment of Chile.Crossref | GoogleScholarGoogle Scholar |

May R, South Australian Research and Development Institute, Rural Solutions SA, Grains Research and Development Corporation (Australia) (2006) ‘Clay spreading and delving on Eyre Peninsula: a broadacre clay application manual for farmers, contractors and advisors.’ (South Australian Research and Development Institute: Adelaide, S. Aust.)

Nang DN (2012) Plant availability of water in soils being reclaimed from the saline-sodic state. PhD Thesis, University of Adelaide, Adelaide, S. Aust.

National Committee on Soil and Terrain (2009) ‘Australian soil and land survey field handbook.’ 3rd edn. (CSIRO Publishing: Melbourne)

Or D, Wraith JM, Robinson DA, Jones SB (2012) Soil water content and water potential relationships. In ‘Handbook of soil sciences: properties and processes’. 2nd edn. (Eds PM Huang, Y Li, ME Sumner) pp. 4-1–4-28. (CRC Press: Boca Raton, FL)

Parametric Technology Corporation (2007) ‘Mathcad 14.’ (Parametric Technology Company: Needham, MA, USA) Available at: www.ptc.com.

Rawls WJ, Brakensiek DL, Saxton KE (1982) Estimation of soil-water properties. Transactions of the American Society of Agricultural Engineers 25, 1316–1328.

Rayment GE (1992) ‘Australian laboratory handbook of soil and water chemical methods.’ (Eds GE Rayment, FR Higginson) (Inkata Press: Melbourne)

Rebbeck M, Lynch C, Hayman PT, Sadras VO (2007) Delving of sandy surfaced soils reduces frost damage in wheat crops. Australian Journal of Agricultural Research 58, 105–112.
Delving of sandy surfaced soils reduces frost damage in wheat crops.Crossref | GoogleScholarGoogle Scholar |

Reynolds WD, Bowman BT, Brunke RR, Drury CF, Tan CS (2000) Comparison of tension infiltrometer, pressure infiltrometer, and soil core estimates of saturated hydraulic conductivity. Soil Science Society of America Journal 54, 1233–1241.

Rijtema PE (1969) Soil moisture forecasting. ICW Report No. 513. Instituut voor Cultuurtechniek en Waterhuishouding. University of Wageningen, Wageningen, The Netherlands.

Ritsema CJ, Dekker LW (2000) Preferential flow in water repellent sandy soils: principles and modeling implications. Journal of Hydrology 231–232, 308–319.
Preferential flow in water repellent sandy soils: principles and modeling implications.Crossref | GoogleScholarGoogle Scholar |

Saxton KE, Rawls WJ (2006) Soil water characteristic estimates by texture and organic matter for hydrologic solutions. Soil Science Society of America Journal 70, 1569–1578.
Soil water characteristic estimates by texture and organic matter for hydrologic solutions.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BD28Xpsl2lsL4%3D&md5=13535e257efc27595211aec72a305cf3CAS |

Shiel RS, Adey MA, Lodder M (1988) The effect of successive wet/dry cycles on aggregate size distribution in a clay texture soil. Journal of Soil Science 39, 71–80.
The effect of successive wet/dry cycles on aggregate size distribution in a clay texture soil.Crossref | GoogleScholarGoogle Scholar |

Smith LH, Tiller KG (1977) A modified procedure for the more rapid determination of the clay content of soils. Divisional Report No. 19. CSIRO Division of Soils.

Tennant D, Scholz G, Dixon J, Purdie B (1992) Physical and chemical characteristics of duplex soils and their distribution in the south-west of Western Australia. Australian Journal of Experimental Agriculture 32, 827–843.
Physical and chemical characteristics of duplex soils and their distribution in the south-west of Western Australia.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DyaK2cXot1Skug%3D%3D&md5=8ef096192c46d01ecfbc11a6a9f20cdfCAS |

van Lier QJ, Metselaar K, van Dam JC (2006) Root water extraction and limiting soil hydraulic conditions estimated by numerical simulation. Vadose Zone Journal 5, 1264–1277.
Root water extraction and limiting soil hydraulic conditions estimated by numerical simulation.Crossref | GoogleScholarGoogle Scholar |

Ward PR (1993) Generation of water repellence in sands, and its amelioration by clay addition. PhD Thesis, University of Adelaide, Adelaide, S. Aust.

WRB IWG (2007) ‘World Reference Base for Soil Resources 2006. First update 2007.’ (FAO: Rome) Available at: www.fao.org