La Sparrow

Soil phosphorus–crop response calibration relationships and criteria for winter cereal crops grown in Australia

Abstract. Soil testing is the most widely used tool to predict the need for fertiliser phosphorus (P) application to crops. This study examined factors affecting critical soil P concentrations and confidence intervals for wheat and barley grown in Australian soils by interrogating validated data from 1777 wheat and 150 barley field treatment series now held in the BFDC National Database. To narrow confidence intervals associated with estimated critical P concentrations, filters for yield, crop stress, or low pH were applied. Once treatment series with low yield (<1 t/ha), severe crop stress, or pHCaCl2 <4.3 were screened out, critical concentrations were relatively insensitive to wheat yield (>1 t/ha). There was a clear increase in critical P concentration from early trials when full tillage was common compared with those conducted in 1995–2011, which corresponds to a period of rapid shift towards adoption of minimum tillage. For wheat, critical Colwell-P concentrations associated with 90 or 95% of maximum yield varied among Australian Soil Classification (ASC) Orders and Sub-orders: Calcarosol, Chromosol, Kandosol, Sodosol, Tenosol and Vertosol. Soil type, based on ASC Orders and Sub-orders, produced critical Colwell-P concentrations at 90% of maximum relative yield from 15 mg/kg (Grey Vertosol) to 47 mg/kg (Supracalcic Calcarosols), with other soils having values in the range 19–27 mg/kg. Distinctive differences in critical P concentrations were evident among Sub-orders of Calcarosols, Chromosols, Sodosols, Tenosols, and Vertosols, possibly due to differences in soil properties related to P sorption. However, insufficient data were available to develop a relationship between P buffering index (PBI) and critical P concentration. In general, there was no evidence that critical concentrations for barley would be different from those for wheat on the same soils. Significant knowledge gaps to fill to improve the relevance and reliability of soil P testing for winter cereals were: lack of data for oats; the paucity of treatment series reflecting current cropping practices, especially minimum tillage; and inadequate metadata on soil texture, pH, growing season rainfall, gravel content, and PBI. The critical concentrations determined illustrate the importance of recent experimental data and of soil type, but also provide examples of interrogation pathways into the BFDC National Database to extract locally relevant critical P concentrations for guiding P fertiliser decision-making in wheat and barley.

Effects of agricultural management on sodosols in northern Tasmania

Attributes of 25 Tasmanian sodosols were assessed using field and laboratory techniques to determine changes associated with 4 typical forms of agricultural management [long-term pasture, cropping with shallow tillage using discs and tines, cropping (including potatoes) with more rigorous and deeper tillage including deep ripping and powered implements, and cropping (including potatoes) where the potatoes were harvested when the soil was wet]. Soil organic carbon in the top 150 mm was 2.7% under long-term pasture compared with 1.8% in rigorously tilled cropping paddocks, and microbial biomass C values were 194 and 129 mg/kg, respectively. Readily oxidisable organic C concentrations were 1.8 mg/g and 1.3 mg/g, respectively. Infiltration rate was greater in paddocks with shallow tillage cropping than long-term pasture but was 43% less in paddocks which had grown potatoes and 70% less after a wet potato harvest. Dry aggregate-size showed no change under shallow tillage cropping compared with long-term pasture but decreased significantly in more rigorously tilled potato cropping paddocks. Aggregate stability in all cropped paddocks was nearly 50% less than in long-term pasture paddocks, with values in intensively tilled potato cropping paddocks approaching relatively low levels. Colwell extractable phosphorus (P) increased with all cropping, particularly after potatoes. Lower organic carbon and poorer physical properties were associated with paddocks which had grown potatoes, which adds weight to the view that cropping rotation and associated soil management practices are critical for sustainable management of Tasmanian sodosols. Farmers were surveyed about their views of the condition of their paddocks. They identified more healthy than unhealthy soil attributes under all management histories but reported more unhealthy soil attributes when potatoes were included in their rotation.

Crop yields and soil properties on eroded slopes of red ferrosols in north-west Tasmania

The differences in soil properties and crop yield on slopes of varying steepness in intensively cropped paddocks with red ferrosols (Humic Eutrodox), which had evidence of erosion over many years, were determined at 5 sites in north-west Tasmania. We found that soils on the steeper slopes, which have had greater soil loss, had significantly lower topsoil carbon concentrations than soils on flatter slopes. We found that significant redistribution of soil had occurred on the sites in this study. Areas with concave slope positions had over-thickened topsoils. However, the effect of erosion on the topsoil thickness of eroded slope positions was masked by the uniform depth of cultivation across paddocks. Penetration resistance increased gradually with depth on all transects, indicating no compacted layers or plough pans on these intensively cropped sites. Soil physical properties did not significantly change from non-eroded, level areas to steep, eroded parts of the paddocks, even although considerable soil loss had occurred from the steep slopes. We attribute this to the gradational nature of these red ferrosols, which characteristically have strongly structured subsoils. Crop yield was significantly correlated with slope but was not significantly different on land up to 18% slope. We anticipate that continued erosion at current rates on this less steep land will inevitably reduce crop yields. We found a significant correlation between organic carbon, total exchangeable bases, extractable K, and crop yield, but no correlation between available water content and crop yield. We conclude that soil organic matter contributes to productivity through its effect on nutrient concentrations. Total exchangeable bases appeared to provide the best and simplest explanatory model to predict crop yield. We propose a set of 4 tests for future assessment of soil condition on these red ferrosols.

Manganese oxidation and reduction in soils: effects of temperature, water potential, pH and their interactions

Manganese (Mn) toxicity is a potential limitation to plant growth on acidic and poorly drained soils. Five laboratory experiments using such soils were conducted to examine the influence of soil temperature, pH and water potential on the redox reactions of Mn and the potential for Mn toxicity. The microbial inhibitor sodium azide was used in some experiments to assess the role of microorganisms in these reactions. The reduction of Mn oxides (MnOx) during waterlogging was faster at 20°C and 30°C than at 10°C or 4°C. Sodium azide slowed the reduction of Mn oxides at 20°C and 30°C during waterlogging but had little effect at 4°C and 10°C, suggesting that microbial MnOx reduction during waterlogging was minimal at the lower temperatures. Re-oxidation of Mn2+ in soil drained after severe waterlogging was only observed in soil not treated with sodium azide, indicating that even when very high concentrations of Mn2+ were present, Mn2+ oxidation was still microbial. Prior liming of aerobic soil established lower starting concentrations of water-soluble plus exchangeable (WS+E) Mn2+ and slowed the reduction of Mn oxides during subsequent waterlogging. After drainage, rapid re-oxidation of Mn2+ was observed in all lime treatments but was fastest at the two highest lime rates. In the fourth and fifth experiments, interactions between temperature and water potential were observed. When waterlogged soils were drained to –5 and –10 kPa, re-oxidation of Mn2+ occurred at both 10°C and 20°C. At –1 kPa, there was no net change in WS+E Mn2+ at 10°C, whereas at 20°C, the concentration of WS+E Mn2+ increased, possibly due to the lower concentration of O2 in the soil water at the higher temperature. In the fifth experiment, at 4°C and 10°C there was little or no effect on Mn reactions of varying water potential from –1 to –1500 kPa, but at 20°C and especially at 30°C, both Mn2+ oxidation and Mn oxide reduction were slowed at –1500 kPa compared with the higher water potentials. Overall, the experiments show that a delicate balance between the microbial oxidation of Mn2+ and the reduction of Mn oxides can exist, and that it can be shifted by small changes in soil water potential along with changes in temperature and pH.

Effects of agricultural management on Vertosols in Tasmania

Attributes of 21 Vertosols in 2 different regions of Tasmania were assessed using field and laboratory techniques to determine differences associated with 3 local forms of agricultural management (long-term pasture, rain-fed cropping, and irrigated cropping). Vertosols in the northern Midlands had better physical properties (lesser bulk density and penetration resistance, and greater porosities and water holding capacities), poorer nutrient status (lower pH, exchangeable bases, and extractable P), and better biological properties (greater organic carbon (OC), carbon fractions F1 and F3, and more worms) than south-eastern Vertosols. When adjusted for clay content, cropped sites had less soil OC than pasture sites at 0-75 mm depth. Readily oxidisable (fraction F1) carbon in the surface 75 mm was 3.6 mg/g and 6.9 mg/g under long-term pasture compared with 2.5 mg/g and 3.9 mg/g in irrigated cropped paddocks on south-eastern and Midlands sites, respectively. Soil organic carbon values were positively correlated with physical and chemical soil properties. Long-term pasture paddocks showed stronger structural development and had smaller aggregates than cropped paddocks, which had more larger clods. Vane shear strength and penetration resistance were less in rainfed cropped paddocks compared with long-term pasture but this effect was not apparent on irrigated cropped paddocks. Farmers considered that a majority of their soil attributes were healthy under all management histories but strategies for maintaining organic matter levels and minimising clod formation by tillage are essential for long-term sustainable use of these Vertosols.

Linking Tasmanian potato and poppy yields to selected soil physical and chemical properties

Selected soil properties and paddock management characteristics were measured for 121 potato and poppy crops in north and northwest Tasmania to see if variation in these characteristics explain variation in crop yield. The soil properties we selected were those that previous work found had changed the most as a result of cropping and, therefore, may be affecting yield on the particular soil type. The soil properties and management characteristics that were significantly correlated with crop yield varied with crop and soil type. None of the soil characters had correlation coefficients greater than 0.63, probably reflecting the capacity of individual farmers to overcome particular soil limitations through their management of tillage, nutrition, irrigation, weeds and pathogens. On ferrosols, a visual score of soil structure was significantly correlated with potato yield (r = 0.57) and exchangeable aluminium was significantly correlated with poppy yield (r = 0.63). Exchangeable calcium (r = 0.54) and penetration resistance (r = 0.38) correlated positively and topdressed nitrogen (r = –0.49) correlated negatively with poppy alkaloid assay, an important determinant of overall poppy yield. On dermosols, depth to 2000 kPa penetration resistance (r = 0.60) and fertiliser P (r = –0.67) were correlated with potato yield, structure score correlated with poppy yield (r = 0.59), and penetration resistance with poppy assay (r = 0.52). On sodosols, fertiliser K (r = –0.41 and r = 0.55) and N (r = –0.45 and 0.42) correlated negatively with poppy yield and positively with poppy assay. On clay loam soils such as dermosols and ferrosols, increased topsoil cloddiness appears to be having a deleterious effect on crop yield. Cloddiness is readily assessed on these soils using the structure scorecard, which could therefore become a practical diagnostic test for farmers and advisers.

Managing and Monitoring Viral and Soil-Borne Pathogens in Tasmanian Potato Crops

The characteristics of Tasmanian potato production, including its geographic isolation, seed certification scheme, and long rotations have helped to minimize the incidence of important potato viruses. However, many soil-borne pathogens have steadily built-up in Tasmanian potato soils. The main influence on pathogen concentrations, especially for the powdery scab pathogen, seems to be the presence of the host crop in the rotation. A useful predictive relationship between pathogen DNA and powdery scab severity has emerged from work to date but needs testing across a range of potato cultivars.

Plant growth and soil responses to soil applied organic materials in Tasmania, Australia

Biosolids, poppy mulch (PM), and poppy seed waste (PSW) were applied to soils in barley and wheat field trials in two areas of Tasmania to determine crop and soil responses and the potential for these materials to substitute for inorganic fertiliser. Lime-amended biosolids (LAB) was applied at one, two, and five times the nitrogen-limiting biosolids application rate (NLBAR). Anaerobically digested biosolids (ADB) was applied at the NLBAR, and PM and PSW were applied at industry-recommended rates. The results indicated that ADB, LAB, PM, and PSW can substitute for inorganic fertiliser in meeting plant nutrient requirements but may be releasing more plant-available N than guideline assumptions. However, organic amendments are less easily managed and applied than inorganic fertiliser, and release of plant-available N from organic amendments may be too rapid for plant uptake to prevent leaching losses. LAB can also leave elevated residual extractable phosphorus in soil after two cereal crops, and PM and LAB can increase soil pH. Microbial biomass showed an inconsistent, and in some cases unexpected, response to organic amendments after 1 year and no significant relationship to changes in soil carbon.

Decrease in phosphorus concentrations when P fertiliser application is reduced or omitted from grazed pasture soils

Many intensively managed soils contain phosphorus (P) concentrations greater than required for optimum production. Soils with P concentrations in excess of the agronomic optimum can have unnecessary losses of P that can adversely affect water bodies. Reducing excessive soil-P concentrations is important for the economic and environmental sustainability of intensive agriculture, such as the Australian dairy industry. However, little is known of decreases in extractable soil-P concentrations when P fertiliser applications are reduced or omitted from soils with P concentrations and properties representative of intensive pasture grazing systems. Decreases in extractable P (calcium chloride (CaCl2), Olsen and Colwell) were monitored for up to 4.5 years for six Australian grazed pasture soils (Red Ferrosol, Brown Kurosol, Grey Dermosol, Brown Dermosol, Podosol and Hydrosol) with contrasting textures and P-buffering indices (PBI). Sixteen treatments consisting of four initial extractable-P concentrations (Pinit) paired with four ongoing P fertiliser rates (Pfert) were established for each of the six soils, except on an extremely low-PBI Podosol, where a range of Pinit concentrations could not be established. The resultant decreases in P were larger with higher Pinit concentration and lower rate of ongoing Pfert, except in the extremely low PBI Podosol where decreases in initially high CaCl2-P concentrations were large irrespective of ongoing Pfert. There was a greater proportional decrease in the environmentally extractable P compared with agronomically extractable P, with mean decreases in CaCl2-P of 57%, Olsen-P of 25%, and Colwell-P of 12%. The Pinit concentrations, which were well above agronomic optimum, remained above this target. This study advances scientific knowledge of extractable soil-P concentrations when P fertiliser inputs are withheld or reduced from grazed pasture soils, and aids land and catchment managers in estimating likely changes over time.

Safeguarding Soil and Water Quality

Abstract In many countries, community awareness and concern about environmental issues has resulted in an increased interest in and requirement for assessment and monitoring of soil and water quality. This paper reviews the types of indicators which are commonly advocated for these purposes, and concludes that better interpretive guidelines for indicators are needed if these guidelines are to be defensible. More work also needs to be done to decrease the cost of appropriate monitoring and to encourage its wider and more intense use. Recent developments in new techniques, and community‐based monitoring programmes in Australia are discussed. Active and well targeted assessment and monitoring programmes by themselves are not sufficient to safeguard soil and water quality. Increased emphasis needs to be given to the development of new land use systems and practices, which address the environmental priorities identified through assessment and monitoring, and which also ensure the financial viability of land managers. Scientists have important roles to play in all of the above processes. Research is one important role, but there is much to be gained from scientists facilitating communication between land managers and policy makers. These gains include the advancement of reforms to land management which have the potential to safeguard soil and water quality, and which are likely to be adopted by land managers and local communities.