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A Revolution in Land Use


Options and future prospects – part 1

Annual cropping

Joint Venture Agroforestry Program

Opportunity cropping

Phase farming

Companion farming

New agricultural plants

Redesigning Agriculture for Australian Landscapes

Organic farming


Annual cropping

Most of the Basin with rainfall greater than 400 mm has been cleared for agriculture, predominantly for annual crops and pastures. In this section we present an overview of the expected leakage of water below annual crops across the Basin. The estimates below are from field-calibrated simulation modelling of annual cropping, but the same principles apply to annual plant-based pasture systems.

Two transects are explored (Figure 8). The first considers the amount of rainfall; the second the timing of rainfall. These simulations are for a deep well-drained soil using weather data collected over the past 40 years.

Figure 8. Simulations were carried out across N–S and E–W transects.

Figure 8. Simulations were carried out across N–S and E–W transects.

The E–W transect runs across the Basin at approximately 33oS, taking in towns such as Condobolin, Parkes and Orange. Annual rainfall ranges from 320 mm in the west to 870 mm in the east. Rainfall at this latitude is slightly winter dominant (55% of the annual total).

The estimates of average annual leakage for a wheat cropping system increase from almost nothing in the west to well over 200 mm in the east (Figure 9). The simulations also show that higher input farming has had a large effect on yield, but not on drainage. Doubling nitrogen fertiliser (N) from 40 to 80 kg/ha increased yield by 20–40% but only reduced annual leakage by about 25 mm (Figure 9). Bigger crops with more leaves mean more transpiration and interception, but this is largely at the expense of soil evaporation, not leakage below the root zone.

Figure 9. Predicted leakage with increasing rainfall along the E–W transect for a range of current land-use options and future prospects.

Figure 9. Predicted leakage with increasing rainfall along the E–W transect for a range of current land-use options and future prospects.

The N–S transect, which explores the impact of winter and summer rainfall dominance, runs roughly along the 575 mm rainfall isohyet (range 550–600 mm), extending from Roma in Queensland, through Moree, Dubbo and Parkes in New South Wales, and ending with Rutherglen and Bendigo in Victoria. The proportion of annual rainfall received in the winter months increased from 40% in Queensland to 70% in Victoria.

The N–S transect highlights the influence of winter-dominant rainfall on leakage (Figure 10). As winter dominance increases, so too does the leakage associated with annual cropping. This is because more of the rainfall occurs in the cooler part of the year, when potential water use by vegetation and loss via soil evaporation is reduced.

While the targets for leakage will need to be specific to catchments or landscapes, they are almost certainly well below 20 mm/y. Therefore, based on these simulations and complementary experimental work, annual cropping systems fall a long way short of acceptable leakage targets. Yet some would argue that this is not the last word.

There has been continuous change in farming systems since the land was first cleared. In trials across southern NSW, wheat crops grown under practices common in the 1990s were compared to a best management package that included disease-break crops or nitrogen top-dressed crops. The better managed crops had higher yield and also left the soil around 20 mm drier. Such improvements are in line with model predictions shown in Figure 9, and again fall short of what is required over most of the cropping zone.

The best hopes for cropping systems are to concentrate on soils with high water-holding capacity, and to introduce summer crops or perennial pastures into rotations according to the amount of water stored in the soil.

Figure 10. Predicted leakage with increasing winter dominance for a range of current land use options and for future prospects (see key Figure 9).

Figure 10. Predicted leakage with increasing winter dominance for a range of current land use options and for future prospects (see key Figure 9).

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Joint Venture Agroforestry Program
(RIRDC/LWRRDC/FWPRDC)

Since 1993, JVAP has led Australia in the development and dissemination of research and practical information to underpin new sustainable farming systems incorporating perennial woody vegetation.

The program focuses on commercially driven tree production systems for addressing land degradation issues. It is developing new treebased industries for integration into low to medium rainfall farming systems. The program aims to deliver cost-effective multi-purpose agroforestry systems to meet commercial and environmental objectives.

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Opportunity cropping

One option to increase water use by annual cropping systems is to sow crops opportunistically in both winter and summer, when rainfall and soil water conditions allow. This is a useful strategy, particularly in the northern half of the Basin, when summer rainfall is more significant and soil water storage generally greater (Figures 9, 10).

In the northern part of the Basin, soils with high water-holding capacity coincide with sufficient summer rain to allow cropping at almost any time of the year. The modelled volume of drainage from a catchment under current management was nearly six times that of the native vegetation. Opportunity cropping yields a leakage volume less than twice that of native vegetation (Figure 11). However, on soils formed from sedimentary rocks, the difference between current and best practice is smaller, and both leak considerably more than the native system.

Figure 11. Modelled leakage under current practice, best practice and the native vegetation in a catchment in northern NSW.

Figure 11. Modelled leakage under current practice, best practice and the native vegetation in a catchment in northern NSW.

Source: Ringrose-Voase and Cresswell (2000)

The greatest obstacle to controlling leakage in annual cropping systems is season-to-season variability in rainfall. Average leakage may be 50 mm/y, but developing farming systems that use an extra 50 mm/y would not solve the problem. The wetter-than-average years contribute most to drainage and any sustainable system must have the capacity to deal with such years. This can only be achieved using perennials.

Annual crops can be made to behave in a more perennial fashion using phase farming or companion farming, combining and alternating perennials with annual crops.

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Phase farming

In phase farming, a deep-rooted perennial like lucerne can create a dry soil buffer of 200 mm or more. This means that it can prevent leakage most years, and also protect subsequent crops in a rotation. The introduction of a perennial deep-rooted pasture phase that can dry the soil to 3 m depth into a cropping rotation (three years pasture followed by three years wheat) across the 575 mm isohyet, drops leakage by 70% or more (Figure 10).

A key element of farming system design that controls leakage is the ability to cope with rainfall variability. For instance, long-term simulation of continuous cropping in central NSW, with 614 mm annual rainfall, produced an average leakage of 107 mm. In 31% of years, the leakage was less than 50 mm, so the cropping phase could occur for at least four years after lucerne. However, in 17% of years, the annual drainage was greater than 200 mm. Such a year, coinciding with a depleted buffer, would lead to unacceptably high leakage (Figure 12).

Figure 12. The modelled probability of getting different amounts of leakage under continuous cropping in central NSW.

Figure 12. The modelled probability of getting different amounts of leakage under continuous cropping in central NSW.

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Companion farming

Companion farming is an emerging concept in which annual cereals are oversown into a perennial pasture system, ideally one that exhibits a strong degree of winter and spring dormancy. The perennial pastures may be native grasslands, like those being trialed by innovative farmers in northern NSW, or deep-rooted legumes such as lucerne or other novel species. Oversowing annuals into winter dormant perennial pastures may be a way of getting around the issue of yearto- year variability in leakage and the technical difficulty of changing phase.

These systems have been explored in calibrated simulation models (see Figures 9, 10) and appear to be potentially more effective than phase farming in controlling leakage, with at least the same grain-yield production possibilities. However, there may be a trade-off in production through competition for water and problems with obtaining a clean harvest.

This option could be implemented over the short term (three to five years), with well-targeted on-farm research and development.

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New agricultural plants

Our current crop and forage species have been bred and/or selected for yield and desirable agronomic characters. Little or no attention has been given to their ability to use water and nitrogen and restrict dryland salinisation.

The immediate opportunities lie in longer season cultivars and species. Good prospects exist to develop winter wheat and canola varieties that can be sown as early as February, if rainfall conditions allow, and grazed in May. They then regrow to produce a grain yield over the normal spring–early summer period.

Longer term, opportunities lie in the use of both improvements in conventional plants and developments in biotechnology to develop new plants with more extensive root systems, greater perenniality, and different degrees of winter and summer activity. Other traits such as enhanced early vigour, waterlogging tolerance and disease resistance would also improve their use of water.

It may be possible to add 'resurrection genes' to annual crops, giving them the ability to re-sprout after harvest in the event of summer rain. At the extreme, it might even be possible to produce perennial grain crops, although it is highly likely that there will be a trade-off between productivity and persistence. This research frontier has been examined as part of a new research and development program entitled 'Redesigning Agriculture for Australian Landscapes' (see below). Some results can be expected in the next five years, but most of the developments mentioned above will require 5 to 25 years of focused research.

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Redesigning Agriculture for Australian Landscapes

The Redesigning Agriculture for Australian Landscapes (RAAL) Research and Development Program is a joint initiative of the Land and Water Resources Research and Development Corporation and CSIRO. The program is researching how agricultural systems in Australia can be redesigned to address a range of sustainability issues. It has four objectives:

  • To understand, by comparison, the key biophysical processes affecting leakage of water and nutrients in cropping, grazing and natural systems.
  • To benchmark criteria for redesigning agricultural systems in Australian landscapes.
  • To develop a toolbox of redesign options to modify current, or develop new, agricultural systems for Australian landscapes.
  • To facilitate implementation of redesign options in priority Australian landscapes by exploring the socio-economic, institutional, policy, marketing and technological requirements and implications of each option.

This design approach has potential to be applied through:

  • selection and plant breeding — including molecular genetics — for our commercial crops, pastures and native plants to manipulate their phenology, canopy development, rooting function, distribution and temperature response.
  • rotating and mixing, in space and time, innovative configurations of plants including: annual and perennial crops, pastures, forest and horticultural trees, native plants and bush foods, in alleys, blocks, windbreaks and clusters, over rotations of months or years.

Recognising the diverse skills and inputs necessary to achieve its mission and objectives, the RAAL Program will actively seek opportunities to collaborate, focusing on:

  • integrating RAAL with a range of other redesign initiatives, and
  • incorporating RAAL outputs into other research and development initiatives.

 

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Organic farming

Organic farming is increasing in importance due to rapidly growing market preference. Organic farming uses crop rotations and diversity to replace agrochemicals, but this does not necessarily mean a shift to greater use of perennial plants. A similar reliance on annual species will expose organic farming to the same risk of leakage as conventional agriculture. Research to give greater emphasis to deep-rooted perennials in phase planting or as companion plants is attractive because organic farmers are well disposed towards and skilled in the complexities of crop/pasture/tree management.

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