Register      Login
Crop and Pasture Science Crop and Pasture Science Society
Plant sciences, sustainable farming systems and food quality
RESEARCH ARTICLE (Open Access)

Hydrological and water-use efficiency implications of geomorphological stratification in palæochannels in the Northern Murray–Darling Basin

C. P. Vanags A C and R. W. Vervoort B C
+ Author Affiliations
- Author Affiliations

A School for Science and Math, Vanderbilt University, Tennessee 37206, USA.

B Hydrology and Geo-Information Sciences Laboratory, Faculty of Agriculture and Environment, The University of Sydney, NSW 2006, Australia.

C Corresponding authors. Emails: willem.vervoort@sydney.edu.au; chris.vanags@vanderbilt.edu

Crop and Pasture Science 64(12) 1182-1194 https://doi.org/10.1071/CP13168
Submitted: 13 May 2013  Accepted: 13 September 2013   Published: 11 November 2013

Journal Compilation © CSIRO Publishing 2013 Open Access CC BY-NC-ND

Abstract

Regional climactic variability coupled with an increasing demand on water has placed an even greater pressure on managers to understand the complex relationships between surface water and groundwater in the Murray–Darling Basin. Based on limited soil sampling combined with geophysical observations, past research has suggested that relic subsurface drainage features (also known as palæochannels) have a higher risk of deep drainage and lateral flow, particularly where water is impounded or applied as irrigation. The aim of this study was to investigate the hydrological behaviour of an irrigated 25-ha site in North-western New South Wales in more detail to predict deep drainage risk in the presence of palæochannel systems. Several years of direct and indirect observations, including soil sampling and groundwater measures, were collected. Coupling the field data with one- and two-dimensional water balance models revealed a more complex behaviour where a palæochannel functions like a large underground drain. In contrast to other studies, this study suggests that the actual palæochannel does not pose a higher drainage risk, but the combination of the palæochannels with the surroundings soils does have a higher deep drainage risk.

Additional keywords: deep drainage risk, groundwater, palæochannel, soil data, water balance modelling.


References

ABS (2008) ‘Water and the Murray–Darling Basin – a statistical profile, Australia 2000–06.’ (Australian Bureau of Statistics: Canberra)

Acworth RI, Timms WA (2009) Evidence for connected water processes through smectite-dominated clays at Breeza, New South Wales. Australian Journal of Earth Sciences 56, 81–96.
Evidence for connected water processes through smectite-dominated clays at Breeza, New South Wales.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BD1MXkvVWks7c%3D&md5=56d5b6cf7cea4719a53fd3cbed373a07CAS |

Asseng S, Fillery IRP, Dunin FX, Keating BA, Meinke H (2001) Potential deep drainage under wheat crops in a Mediterranean climate. I. Temporal and spatial variability. Australian Journal of Agricultural Research 52, 45–56.
Potential deep drainage under wheat crops in a Mediterranean climate. I. Temporal and spatial variability.Crossref | GoogleScholarGoogle Scholar |

Booltink HWG, van Breemen N, Bongers N, Waringa N, van Grinsven JJM, Dirksen C (1988) Automated in situ measurement of unsaturated soil water flux. Soil Science Society of America Journal 52, 1215–1218.
Automated in situ measurement of unsaturated soil water flux.Crossref | GoogleScholarGoogle Scholar |

Fetter CW (2001) ‘Applied hydrogeology.’ 4th edn. (Prentice Hall: Upper Saddle River, NJ)

Flury M, Fluhler H, Jury WA, Leuenberger J (1994) Susceptibility of soils to preferential flow of water: a field study. Water Resources Research 30, 1945–1954.
Susceptibility of soils to preferential flow of water: a field study.Crossref | GoogleScholarGoogle Scholar |

Gee GW, Bauder JW (1986) Particle size analysis. In ‘Methods of soil analysis. Part 1 – physical and mineralogical methods’. (Ed. A Klute) pp. 383–411. (American Soil Science Society: Madison, WI)

Glendenning CJ, Vervoort RW (2010) Hydrological impacts of rainwater harvesting (RWH) in a case study catchment: the Arvari River, Rajasthan, India. Part 1: field-scale impacts. Agricultural Water Management 98, 331–342.
Hydrological impacts of rainwater harvesting (RWH) in a case study catchment: the Arvari River, Rajasthan, India. Part 1: field-scale impacts.Crossref | GoogleScholarGoogle Scholar |

Gunawardena TA, McGarry D, Robinson JB, Silburn DM (2011) Deep drainage through Vertosols in irrigated fields measured with drainage lysimeters. Soil Research 49, 343–354.
Deep drainage through Vertosols in irrigated fields measured with drainage lysimeters.Crossref | GoogleScholarGoogle Scholar |

Hendrickx JMH, Phillips FM, Harrison JB (2003) Water flow processes in arid and semi-arid vadose zones. In ‘Understanding water in a dry environment’. (Ed. I Simmers) pp. 151–204. (A. A. Balkema Publishers: Lisse, The Netherlands)

Hsieh PA, Wingle W, Healy RW (2000) ‘VS2DI – a graphical software package for simulating fluid flow and solute or energy transport in variably saturated porous media.’ USGS, No. 99-4130. (USGS: Lakewood, CO)

Huckel AI (2001) Estimating clay content and deep drainage at the field scale in the lower Gwydir River Valley. MSc Agric. Thesis, The University of Sydney, NSW, Australia.

Hulugalle NR, Weaver TB, Finlay LA (2012) Soil water storage, drainage, and leaching in four irrigated cotton-based cropping systems sown in a Vertosol with subsoil sodicity. Soil Research 50, 652–663.
Soil water storage, drainage, and leaching in four irrigated cotton-based cropping systems sown in a Vertosol with subsoil sodicity.Crossref | GoogleScholarGoogle Scholar |

Kroes JG, van Dam JC, Groenendijk P, Hendriks RFA, Jacobs CMJ (2008) ‘SWAP version 3.2: Theory description and user manual.’ Report No. 1649. (Alterra: Wageningen)

Larsson MH, Jarvis NJ (1999) Evaluation of a dual-porosity model to predict field-scale solute transport in a macroporous soil. Journal of Hydrology 215, 153–171.
Evaluation of a dual-porosity model to predict field-scale solute transport in a macroporous soil.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DyaK1MXhtFWmsbw%3D&md5=bdc7ea1d0690fb6945f270177fd32651CAS |

Minasny B, McBratney AB (2003) ‘NeuroTheta, pedotransfer function for predicting soil hydraulic properties for Australian soil.’ (Australian Centre for Precision Agriculture, The University of Sydney: Sydney, NSW)

Nordt LC, Hallmark CT, Wilding LP, Boutton TW (1998) Quantifying pedogenic carbonate accumulations using stable carbon isotopes. Geoderma 82, 115–136.
Quantifying pedogenic carbonate accumulations using stable carbon isotopes.Crossref | GoogleScholarGoogle Scholar |

Page KJ, Nanson GC, Price D (1996) Chronology of Murrumbidgee river palaeochannels on the riverine plain southeastern Australia. Journal of Quaternary Science 11, 311–326.
Chronology of Murrumbidgee river palaeochannels on the riverine plain southeastern Australia.Crossref | GoogleScholarGoogle Scholar |

Petheram C, Walker GR, Grayson RB, Thierfelder T, Zhang L (2002) Towards a framework for predicting impacts of land use on recharge: 1. A review of recharge studies in Australia. Australian Journal of Soil Research 40, 397–417.
Towards a framework for predicting impacts of land use on recharge: 1. A review of recharge studies in Australia.Crossref | GoogleScholarGoogle Scholar |

Philip JR (1969) Hydrostatics and hydrodynamics in swelling soils. Water Resources Research 5, 1070–1077.
Hydrostatics and hydrodynamics in swelling soils.Crossref | GoogleScholarGoogle Scholar |

Quiggin J, Adamson D, Chambers S, Schrobback P (2010) Climate change, uncertainty, and adaptation: the case of irrigated agriculture in the Murray–Darling Basin in Australia. Canadian Journal of Agricultural Economics 58, 531–554.
Climate change, uncertainty, and adaptation: the case of irrigated agriculture in the Murray–Darling Basin in Australia.Crossref | GoogleScholarGoogle Scholar |

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

Ringrose-Voase A, Nadelko T (2011) Deep drainage in a Vertosol under irrigated cotton. In ‘Soil solutions for a changing world. Proceedings 19th World Congress of Soil Science’. (Eds R Gilkes, N Prakongkep) pp. 27–30. (ISSS: Brisbane)

Ritzema HP (Ed.) (1994) Subsurface flow to drains. In ‘Drainage principles and applications’. 2nd edn. Vol. 162. pp. 263–282. (ILRI: Wageningen)

Rogers MP, Christen EW, Khan S (2002) Aquifer identification and characterisation for salinity control by shallow groundwater pumping. CSIRO Land and Water, No. 16/02, Griffith, NSW.

Silburn DM, Tolmie PE, Biggs AJW, Whish JPM, French V (2011) Deep drainage rates of Grey Vertosols depend on land use in semi-arid subtropical regions of Queensland, Australia. Soil Research 49, 424–438.
Deep drainage rates of Grey Vertosols depend on land use in semi-arid subtropical regions of Queensland, Australia.Crossref | GoogleScholarGoogle Scholar |

Smedema LK (1984) Furrow irrigation design for vertisols. Agricultural Water Management 9, 211–218.
Furrow irrigation design for vertisols.Crossref | GoogleScholarGoogle Scholar |

Sophocleous MA (1991) Stream-floodwave propagation through the Great Bend alluvial aquifer, Kansas – field-measurements and numerical simulations. Journal of Hydrology 124, 207–228.
Stream-floodwave propagation through the Great Bend alluvial aquifer, Kansas – field-measurements and numerical simulations.Crossref | GoogleScholarGoogle Scholar |

Stannard ME, Kelly ID (1968) ‘Irrigation potential of the Lower Gwydir Valley.’ (Water Conservation and Irrigation Commission: Sydney)

Talsma T (1977) Measurement of the overburden component of total potential in swelling field soils. Australian Journal of Soil Research 15, 95–102.
Measurement of the overburden component of total potential in swelling field soils.Crossref | GoogleScholarGoogle Scholar |

Timms W, Acworth RI, Berhane D (2001) Shallow groundwater dynamics in smectite dominated clay on the Liverpool Plains of New South Wales. Australian Journal of Soil Research 39, 203–218.
Shallow groundwater dynamics in smectite dominated clay on the Liverpool Plains of New South Wales.Crossref | GoogleScholarGoogle Scholar |

Tolmie PE, Silburn DM, Biggs AJW (2011) Deep drainage and soil salt loads in the Queensland Murray–Darling Basin using soil chloride: comparison of land uses. Soil Research 49, 408–423.
Deep drainage and soil salt loads in the Queensland Murray–Darling Basin using soil chloride: comparison of land uses.Crossref | GoogleScholarGoogle Scholar |

Triantafilis J, Huckel AI, Odeh IOA (2003) Field-scale assessment of deep drainage risk. Irrigation Science 21, 183–192.

Triantafilis J, Odeh IOA, Jarman AL, Short MG, Kokkoris E (2004) Estimating and mapping deep drainage risk at the district level in the lower Gwydir and Macquarie valleys, Australia. Australian Journal of Experimental Agriculture 44, 893–912.
Estimating and mapping deep drainage risk at the district level in the lower Gwydir and Macquarie valleys, Australia.Crossref | GoogleScholarGoogle Scholar |

Vervoort RW, Annen YL (2006) Palaeochannels in Northern New South Wales: inversion of electromagnetic induction data to infer hydrologically relevant stratigraphy. Australian Journal of Soil Research 44, 35–45.
Palaeochannels in Northern New South Wales: inversion of electromagnetic induction data to infer hydrologically relevant stratigraphy.Crossref | GoogleScholarGoogle Scholar |

Vervoort RW, Cattle SR, Minasny B (2003) The hydrology of Vertosols used for cotton production: I Hydraulic, structural and fundamental soil properties. Australian Journal of Soil Research 41, 1255–1272.
The hydrology of Vertosols used for cotton production: I Hydraulic, structural and fundamental soil properties.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BD3sXpsFentLk%3D&md5=b378d0068e7e2c3c64a2ebf8383062adCAS |

Vervoort RW, Minasny B, Cattle SR (2006) The hydrology of Vertosols used for cotton production: II. Pedotransfer functions to predict hydraulic properties. Australian Journal of Soil Research 44, 479–486.
The hydrology of Vertosols used for cotton production: II. Pedotransfer functions to predict hydraulic properties.Crossref | GoogleScholarGoogle Scholar |

Weaver TB, Hulugalle NR, Ghadiri H, Harden S (2013) Quality of drainage water under irrigated cotton in Vertisols of the Lower Namoi Valley, New South Wales, Australia. Irrigation and Drainage 62, 107–114.
Quality of drainage water under irrigated cotton in Vertisols of the Lower Namoi Valley, New South Wales, Australia.Crossref | GoogleScholarGoogle Scholar |

Willis TM, Black AS, Meyer WS (1997) Estimates of deep percolation beneath cotton in the Macquarie valley. Irrigation Science 17, 141–150.
Estimates of deep percolation beneath cotton in the Macquarie valley.Crossref | GoogleScholarGoogle Scholar |

Woodforth A, Triantafilis J, Cupitt J, Malik R, Subasinghe R, Ahmed M, Huckel A, Geering H (2012) Mapping estimated deep drainage in the lower Namoi Valley using a chloride mass balance model and EM34 data. Geophysics 77, WB245–WB256.
Mapping estimated deep drainage in the lower Namoi Valley using a chloride mass balance model and EM34 data.Crossref | GoogleScholarGoogle Scholar |

Wray RAL (2009) Palaeochannels of the Namoi River Floodplain, New South Wales, Australia: the use of multispectral Landsat imagery to highlight a Late Quaternary change in fluvial regime. The Australian Geographer 40, 29–49.
Palaeochannels of the Namoi River Floodplain, New South Wales, Australia: the use of multispectral Landsat imagery to highlight a Late Quaternary change in fluvial regime.Crossref | GoogleScholarGoogle Scholar |

Yoder RE, Freeland RS, Ammons JT, Leonard LL (2001) Mapping agricultural fields with GPR and EMI to identify offsite movement of agrochemicals. Journal of Applied Geophysics 47, 251–259.
Mapping agricultural fields with GPR and EMI to identify offsite movement of agrochemicals.Crossref | GoogleScholarGoogle Scholar |

Young RW, Young ARM, Price DM, Wray RAL (2002) Geomorphology of the Namoi alluvial plain, northwestern New South Wales. Australian Journal of Earth Sciences 49, 509–523.
Geomorphology of the Namoi alluvial plain, northwestern New South Wales.Crossref | GoogleScholarGoogle Scholar |