Water use, competition, and crop production in low rainfall, alley farming systems of south-eastern Australia

2003 ◽  
Vol 54 (8) ◽  
pp. 751 ◽  
Author(s):  
Murray Unkovich ◽  
Kerrin Blott ◽  
Alex Knight ◽  
Ivan Mock ◽  
Abdur Rab ◽  
...  
Keyword(s):  
Soil Water ◽  
Water Use ◽  
Crop Yield ◽  
Farming Systems ◽  
Alley Farming ◽  
Annual Crop ◽  
South Eastern ◽  
Annual Crops ◽  
Eastern Australia ◽  
Perennial Shrubs

Annual crops were grown in alleys between belts of perennial shrubs or trees over 3–4 years at 3 sites across low rainfall (<450 mm) south-eastern Australia. At the two lower rainfall sites (Pallamana and Walpeup), crop grain yields within 2–5 m of shrub belts declined significantly with time, with a reduction equivalent to 45% over 9 m in the final year of cropping. At the third, wetter site (Bridgewater), the reduction in crop grain yields adjacent to tree belts was not significant until the final year of the study (12% over 11 m) when the tree growth rates had increased. The reductions in crop yield were associated with increased competition for water between the shrub or tree belts and the crops once the soil profile immediately below the perennials had dried. At all 3 sites during the establishment year, estimates of water use under the woody perennials were less than under annual crops, but after this, trends in estimates of water use of alley farming systems varied between sites. At Pallamana the perennial shrubs used a large amount of stored soil water in the second summer after establishment, and subsequently were predominantly dependent on rainfall plus what they could scavenge from beneath the adjacent crop. After the establishment year at the Walpeup site, water use under the perennial shrubs was initially 67 mm greater than under the annual crop, declining to be only 24 mm greater in the final year. Under the trees at Bridgewater, water use consistently increased to be 243 mm greater than under the adjacent annual crop by the final year. Although the shrub belts used more water than adjacent crop systems at Walpeup and Pallamana, this was mostly due to the use of stored soil water, and since the belts occupied only 7–18% of the land area, increases in total water use of these alley farming systems compared with conventional crop monocultures were quite small, and in terms of the extent of recharge control this was less than the area of crop yield loss. At the wetter, Bridgewater site, alley farming appeared to be using an increasing amount of water compared with conventional annual cropping systems. Overall, the data support previous work that indicates that in lower rainfall environments (<350 mm), alley farming is likely to be dogged by competition for water between crops and perennials.

Using soil, climate, and agronomy to predict soil water use by lucerne compared with soil water use by annual crops or pastures

2006 ◽  
Vol 57 (3) ◽  
pp. 347 ◽  
Author(s):  
P. R. Ward ◽  
S. F. Micin ◽  
F. X. Dunin
Keyword(s):  
Soil Water ◽  
Water Use ◽  
Plant Density ◽  
Farming Systems ◽  
Summer Rainfall ◽  
Buffer Size ◽  
Rooting Depth ◽  
Regression Equations ◽  
Annual Crops ◽  
Matter Production

The incorporation of perennials in general, and lucerne in particular, into farming systems of southern Australia has been proposed as a possible means to slow or stop the spread of dryland salinity. In order to be effective, lucerne roots must remove substantially more water from the soil than roots produced by annual crops and pastures. The term ‘buffer’ is used here to denote the extra water storage created by lucerne in addition to that normally created by an annual crop or pasture. In trials across southern Australia, lucerne has proved variable in its ability to create a buffer. In this research, we established 3 new trials, and collated results from current and published trials across Australia, to determine the effect of various edaphic (soil pH, texture, depth, and density for A and B horizons), climatic (average and actual seasonal rainfall), and agronomic (lucerne age, plant density, dry matter production, and rooting depth) factors on buffer size created by lucerne. Data from 26 trials were analysed, representing 84 site × year comparisons. The mean lucerne buffer for all comparisons was 91 mm, and increased with lucerne age. Buffers were generally greater for heavier-textured soils, but standard deviations of the means were large. Within a broad soil type, regression equations were developed to predict buffer size from climatic, edaphic, and agronomic factors, with r2 values ranging between 0.96 and 0.84, and standard errors ranging between 40 and 44 mm. For all soil types, average summer rainfall (but not actual summer rainfall) was a significant component of the regression, suggesting that management of the lucerne stand, in terms of maintaining leaf area during summer, may have an important role in buffer development.

Soil water extraction by dryland crops, annual pastures, and lucerne in south-eastern Australia

2001 ◽  
Vol 52 (2) ◽  
pp. 183 ◽  
Author(s):  
J. F. Angus ◽  
R. R. Gault ◽  
M. B. Peoples ◽  
M. Stapper ◽  
A. F. van Herwaarden
Keyword(s):  
Soil Water ◽  
Water Use ◽  
Crop Management ◽  
Water Extraction ◽  
South Eastern ◽  
Eastern Australia ◽  
Soil Water Extraction ◽  
The Mean ◽  
Dryland Crops ◽  
South Eastern Australia

The extraction of soil water by dryland crops and pastures in south-eastern Australia was examined in 3 studies. The first was a review of 13 published measurements of soil water-use under wheat at several locations in southern New South Wales. Of these, 8 showed significantly more water extracted by crops managed with increased nitrogen supply or growing after a break crop. The mean additional soil water extraction in response to break crops was 31 mm and to additional N was 11 mm. The second study used the SIMTAG model to simulate growth and water-use by wheat in relation to crop management at Wagga Wagga. The model was set up to simulate crops that produced either average district yields or the potential yields achievable with good management. When simulated over 50 years of weather data, the combined water loss as drainage and runoff was predicted to be 67 mm/year for poorly managed crops and 37 mm for well-managed crops. Water outflow was concentrated in 70% of years for the poorly managed crops and 56% for the well-managed crops. In those years the mean losses were estimated to be 95 mm and 66 mm, respectively. The third study reports soil water measured twice each year during a phased pasture–crop sequence over 6.5 years at Junee. Mean water content of the top 2.0 m of soil under a lucerne pasture averaged 211 mm less than under a subterranean clover-based annual pasture and 101 mm less than under well-managed crops. Collectively, these results suggest that lucerne pastures and improved crop management can result in greater use of rainfall than the previous farming systems based on annual pastures, fallows, and poorly managed crops. The tactical use of lucerne-based pastures in sequence with well-managed crops can help the dewatering of the soil andreduce or eliminate the risk of groundwater recharge.

scholarly journals Effects of Different Fertilization Regimes on Crop Yield and Soil Water Use Efficiency of Millet and Soybean

2020 ◽  
Vol 12 (10) ◽  
pp. 4125 ◽  
Author(s):  
Qiang Liu ◽  
Hongwei Xu ◽  
Xingmin Mu ◽  
Guangju Zhao ◽  
Peng Gao ◽  
...  
Keyword(s):  
Soil Water ◽  
Water Use ◽  
Crop Yield ◽  
Fertilizer Application ◽  
P Fertilization ◽  
The Loess Plateau ◽  
Total N ◽  
Use Efficiency ◽  
P Application ◽  
Soil Water Consumption

Soil water and nutrients are major factors limiting crop productivity. In the present study, soil water use efficiency (WUE) and crop yield of millet and soybean were investigated under nine fertilization regimes (no nitrogen (N) and no phosphorus (P) (CK), 120 kg ha−1 N and no P (N1P0), 240 kg ha−1 N and no P (N2P0), 45 kg ha−1 P and no N (N0P1), 90 kg ha−1 P and no N (N0P2), 120 kg ha−1 N and 45 kg ha−1 P (N1P1), 240 kg ha−1 N and 45 kg ha−1 P (N2P1), 120 kg ha−1 N and 90 kg ha−1 P (N1P2), 240 kg ha−1 N and 90 kg ha−1 P (N2P2)) in the Loess Plateau, China. We conducted fertilization experiments in two cultivation seasons and collected soil nutrient, water use, and crop yield data. Combined N and P fertilization resulted in the greatest increase in crop yield and WUE, followed by the single P fertilizer application, and single N fertilizer application. The control treatment, which consisted of neither P nor N fertilizer application, had the least effect on crop yield. The combined N and P fertilization increased soil organic matter (SOM) and soil total N, while soil water consumption increased in all treatments. SOM and total N content increased significantly when compared to the control conditions, by 27.1–81.3%, and 301.3–669.2%, respectively, only under combined N and P application. The combined N and P application promoted the formation of a favorable soil aggregate structure and improved soil microbial activity, which accelerated fertilizer use, and enhanced the capacity of soil to maintain fertilizer supply. Crop yield increased significantly in all treatments when compared to the control conditions, with soybean and millet yields increasing by 82.5–560.1% and 55–490.8%, respectively. The combined application of N and P fertilizers increased soil water consumption, improved soil WUE, and satisfied crop growth and development requirements. In addition, soil WUE was significantly positively correlated with crop yield. Our results provide a scientific basis for rational crop fertilization in semi-arid areas on the Loess Plateau.

Improving water use of annual crops and pastures—limitations and opportunities in Western Australia

2001 ◽  
Vol 52 (2) ◽  
pp. 171 ◽  
Author(s):  
David Tennant ◽  
David Tennant ◽  
David Hall ◽  
David Hall
Keyword(s):  
Water Use ◽  
Western Australia ◽  
Chemical Properties ◽  
Farming Systems ◽  
Water Infiltration ◽  
Root Penetration ◽  
Depth Limit ◽  
Annual Crops ◽  
Loamy Sand Soil ◽  
Selection Of

As part of a wider analysis of the potential role for lucerne in farming systems being developed for containing the spread of salinisation, we have reviewed information generated in Western Australia on opportunities for improving the water use of annual crops and pastures. Substantial increases in water use have been shown to be possible in a number of situations and rainfall environments. Best gains, of the order of 40–70 mm, were reported on deep sand and loamy sand soil types. These were achieved from selection of deep-rooted and longer growing crop and pasture species, and from amelioration of widespread traffic pans and subsoil acidity, and/or selection of tolerant species. On more widespread gradational and duplex soils, soil physical and chemical properties that restrict water infiltration and/or root penetration to depth limit the potential to increase water use. Increases in production and water use are still possible, depending on the permeability of the lower horizons of these soils and on rainfall distribution. At best, recorded increases on these soils were of the order of 5–15 mm in short season, low rainfall environments, and around 40 mm in long season, high rainfall environments. These increases in water use were not invariable. Increases in water use were not noted in dry years on all soils and in all years on shallow duplex soils with impermeable B horizons. Seasonality impacts on all outcomes and is a key issue on all soils and in all rainfall environments.

High crop productivity with high water use in winter and summer on the Liverpool Plains, eastern Australia

2008 ◽  
Vol 59 (4) ◽  
pp. 303 ◽  
Author(s):  
R. R. Young ◽  
P.-J. Derham ◽  
F. X. Dunin ◽  
A. L. Bernardi ◽  
S. Harden
Keyword(s):  
Water Use Efficiency ◽  
Soil Water ◽  
Water Use ◽  
High Water ◽  
Crop Productivity ◽  
Transpiration Efficiency ◽  
Eastern Australia ◽  
Use Efficiency ◽  
Water Outflow ◽  
Almost All

We report exceptional productivity and associated water-use efficiency across seasons for commercial crops of rainfed spring wheat and grain sorghum growing on stored soil water in Vertosols on the Liverpool Plains, central-eastern Australia. Agreement between the independently measured terms of evapotranspiration (ET) and the soil water balance (in-crop rainfall + δsoil water) was achieved within acceptable uncertainty across almost all measurement intervals, to provide a reliable dataset for the analysis of growth and water-use relationships without the confounding influence of water outflow either overland or within the soil. Post-anthesis intrinsic transpiration efficiency (kc ) values of 4.7 and 7.2 Pa for wheat and sorghum, respectively, and grain yields of 8 and 7 t/ha from ET of 450 and 442 mm (1.8 and 1.6 g/m2.mm), clearly demonstrate the levels of productivity and water-use efficiency possible for well-managed crops within an intensive and productive response cropping sequence. The Vertosols in which the crops were grown enabled rapid and apparently unconstrained delivery of significant quantities of subsoil water (34% and 51% of total available) after anthesis, which enabled a doubling of pre-anthesis standing biomass and harvest indices of almost 50%. Durum wheat planted into only 0.30 m of moist soil and enduring lower than average seasonal rainfall, yielded less biomass and grain (2.3 t/ha) with lower water-use efficiency (0.95 g/m2.mm) but larger transpiration efficiency, probably due to reduced stomatal conductance. We argue that crop planting in response to stored soil water and management for high water-use efficiency to achieve high levels of average productivity of crop sequences over time can have a significant effect on both increased productivity and enhanced hydrological stability across alluvial landscapes.

Advances in precision agriculture in south-eastern Australia. III. Interactions between soil properties and water use help explain spatial variability of crop production in the Victorian Mallee

2009 ◽  
Vol 60 (9) ◽  
pp. 870 ◽  
Author(s):  
R. D. Armstrong ◽  
J. Fitzpatrick ◽  
M. A. Rab ◽  
M. Abuzar ◽  
P. D. Fisher ◽  
...  
Keyword(s):  
Root Growth ◽  
Grain Yield ◽  
Soil Properties ◽  
Soil Water ◽  
Water Use ◽  
Precision Agriculture ◽  
Crop Growth ◽  
Management Zones ◽  
Eastern Australia ◽  
Supplementary Irrigation

A major barrier to the adoption of precision agriculture in dryland cropping systems is our current inability to reliably predict spatial patterns of grain yield for future crops for a specific paddock. An experiment was undertaken to develop a better understanding of how edaphic and climatic factors interact to influence the spatial variation in the growth, water use, and grain yield of different crops in a single paddock so as to improve predictions of the likely spatial pattern of grain yields in future crops. Changes in a range of crop and soil properties were monitored over 3 consecutive seasons (barley in 2005 and 2007 and lentils in 2006) in the southern section of a 167-ha paddock in the Mallee region of Victoria, which had been classified into 3 different yield (low, moderate, and high) and seasonal variability (stable and variable) zones using normalised difference vegetation index (NDVI) and historic yield maps. The different management zones reflected marked differences in a range of soil properties including both texture in the topsoil and potential chemical-physical constraints in the subsoil (SSCs) to root growth and water use. Dry matter production, grain yield, and quality differed significantly between the yield zones but the relative difference between zones was reduced when supplementary irrigation was applied to barley in 2005, suggesting that some other factor, e.g. nitrogen (N), may have become limiting in that year. There was a strong relationship between crop growth and the use of soil water and nitrate across the management zones, with most water use by the crop occurring in the pre-anthesis/flowering period, but the nature of this relationship appeared to vary with year and/or crop type. In 2006, lentil yield was strongly related to crop establishment, which varied with soil texture and differences in plant-available water. In 2007 the presence of soil water following a good break to the season permitted root growth into the subsoil where there was evidence that SSCs may have adversely affected crop growth. Because of potential residual effects of one crop on another, e.g. through differential N supply and use, we conclude that the utility of the NDVI methodology for developing zone management maps could be improved by using historical records and data for a range of crop types rather than pooling data from a range of seasons.

Water use of wheat, barley, canola, and lucerne in the high rainfall zone of south-western Australia

2005 ◽  
Vol 56 (7) ◽  
pp. 743 ◽  
Author(s):  
Heping Zhang ◽  
Neil C. Turner ◽  
Michael L. Poole
Keyword(s):  
Soil Water ◽  
Water Use ◽  
Western Australia ◽  
Dry Matter ◽  
Grain Filling ◽  
Rooting Depth ◽  
Dry Matter Accumulation ◽  
High Rainfall ◽  
Annual Crops ◽  
Significant Difference

Water use of wheat (Triticum aestivum L.), barley (Hordeum vulgare L.), canola (Brassica napus L.), and lucerne (Medicago sativa L.) was measured on a duplex soil in the high rainfall zone (HRZ) of south-western Australia from 2001 to 2003. Rainfall exceeded evapotranspiration in all years, resulting in transient perched watertables, subsurface waterlogging in 2002 and 2003, and loss of water by deep drainage and lateral flow in all years. There was no significant difference in water use among wheat, barley, and canola. Lucerne used water at a similar rate to annual crops during the winter and spring, but continued to extract 80−100 mm more water than the annual crops over the summer and autumn fallow period. This resulted in about 50 mm less drainage past the root-zone than for annual crops in the second and third years after the establishment of the lucerne. Crop water use was fully met by rainfall from sowing to anthesis and a significant amount of water (120−220 mm) was used during the post-anthesis period, resulting in a ratio of pre- to post-anthesis water use (ETa : ETpa) of 1 : 1 to 2 : 1. These ratios were lower than the indicative value of 2 : 1 for limited water supply for grain filling. High water use during the post-anthesis period was attributed to high available soil water at anthesis, a large rooting depth (≥1.4 m), a high proportion (15%) of roots in the clay subsoil, and regular rainfall during grain filling. The pattern of seasonal water use by crops suggested that high dry matter at anthesis did not prematurely exhaust soil water for grain filling and that it is unlikely to affect dry matter accumulation during grain filling and final grain yield under these conditions.

SPATIAL VARIABILITY IN FOREST WATER USE FROM THREE CONTRASTING REGIONS OF SOUTH-EASTERN AUSTRALIA

2012 ◽  
pp. 233-240 ◽  
Author(s):  
R.G. Benyon ◽  
P.N.J. Lane ◽  
S. Theiveyanathan ◽  
T.M. Doody ◽  
P.J. Mitchell
Keyword(s):  
Spatial Variability ◽  
Water Use ◽  
South Eastern ◽  
Eastern Australia ◽  
South Eastern Australia

Evaluation of chicory cultivars and accessions for forage in south-eastern Australia

2010 ◽  
Vol 61 (7) ◽  
pp. 554 ◽  
Author(s):  
Guangdi D. Li ◽  
Zhongnan Nie ◽  
Amanda Bonython ◽  
Suzanne P. Boschma ◽  
Richard C. Hayes ◽  
...  
Keyword(s):  
South Australia ◽  
Farming Systems ◽  
Wagga Wagga ◽  
Severe Drought ◽  
Climate Conditions ◽  
South Eastern ◽  
Mixed Farming ◽  
South Wales ◽  
Eastern Australia ◽  
South Eastern Australia

The comparative herbage production and persistence of 7 chicory cultivars and 14 accessions collected from diverse regions of the world were evaluated over 3 years in 5 agro-ecological environments across New South Wales (NSW), Victoria (Vic.) and South Australia (SA). Results showed that all cultivars had higher herbage yields than the accessions, but varied greatly among sites. Averaged across all cultivars, total herbage yields were up to 24.6 t DM/ha over 3 years at the Hamilton, Vic. site, but as low as 6.9 and 5.7 t DM/ha at the Wagga Wagga and Bookham, NSW sites, respectively, where chicory only persisted for 2 years. In contrast, the average herbage yield of all accessions was only one-half of that produced by the cultivars at the Hamilton site and about one-third of that at the other 4 sites. All cultivars and accessions persisted well under the favourable climate conditions experienced at the Hamilton site. In contrast, severe drought in 2006 resulted in the death of chicory swards at the Wagga Wagga and Bookham sites, and substantial declines in persistence at the Manilla, NSW and Willalooka, SA sites. Nevertheless, accessions collected from Australia and Asia were more persistent than some of the cultivars and may provide opportunities to select genotypes better adapted to intermittently dry mixed farming systems in south-eastern Australia. Our findings indicated that the current cultivars were best suited to sites similar to the Hamilton site in the winter-dominant, higher rainfall zone of south-eastern Australia. Under these conditions chicory was likely to be productive and persistent for 4 years or longer. In the drier mixed farming zone, chicory may be more suitable in shorter (2–3-year) pasture phases. Further research is required to identify those factors contributing to poor persistence.

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