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MMFS Manual

Chapter 6.3 Test and observe soils for key indicators of soil health

Background information

Standard soil tests can provide a lot of information about your soils and differences between paddocks, no matter what your attitudes and preferences about soil management techniques or fertilisers. Soil nutrient deficiencies and cation imbalances related to soil structure can have a compounding impact — these soils are likely to have poor plant and root growth, low groundcover and litter levels and, therefore, lower water holding capacity and soil organic matter supporting fewer soil organisms such as bacteria, fungi and earthworms.  

In addition to laboratory testing, visual indicators of soil condition, such as pasture discolouration and growth, large bare patches, areas with high weed growth, pooling water, the number of earthworms present, and the look, smell and feel of soil can give important indications of soil health.  

This chapter covers taking a soil test, interpreting the results, and identifying soil health problems such as soil acidity or sodicity.  

Supplying nutrients through fertiliser investment decisions, to maintain or lift pasture growth and maximise profit, are dealt with in Chapter 7.1 in MMFS Module 7 Grow More Pasture. 

At a glance

  • Use soil tests to help monitor nutrient levels and soil health on different areas of your property. 

Soil testing provides a range of information on nutrient levels, conditions and other measures, such as carbon status. Tests can identify if there is an aspect of the soil which is limiting production and also rate soil conditions against industry benchmarks. The results can be used to determine if inputs are required and what nutrient or product can be applied to address the deficiency. Understanding soil test results gives you the confidence to invest in appropriate inputs to address aspects of soil fertility and conditions which can limit production and can help identify which is the most cost-effective product to apply.

Standard soil tests provide an analysis of:

  • Fertility: nitrogen (N), phosphorus (P), sulphur (S) and potassium (K)
  • Soil acidity: pH (usually in calcium chloride (CaCl2) and water), exchangeable aluminium (Al)
  • Salinity: electrical conductivity (EC)
  • Soil structure: texture, colour, organic carbon, calcium:magnesium ratio, exchangeable sodium percentage (ESP)
  • Tests for interpretation of product type and rate: Phosphorus Buffer Index (PBI), cation exchange capacity (CEC)

The three most commonly deficient nutrients are phosphorus, potassium and sulphur.

Phosphorous (P)

Phosphorous is measured as Olsen P or Colwell P. Olsen P measures the amount of nutrient immediately available to plants. Olsen P remains stable throughout the year. Colwell P measures the immediately available phosphorous (Olsen P) plus the phosphorous that is bound to the soil particles and released over time. This means the Colwell P is always higher than the Olsen P. The relationship between Olsen P and Colwell P varies with soil type.

Potassium (K)

Potassium levels are measured using the Colwell K test which identifies the amount of nutrient immediately available to plants and remains relatively stable throughout the year.

Sulphur (S)

Sulphur is assessed using the KCL 40 test which identifies the amount of sulphate sulphur immediately available to the plant. Other sulphur – elemental sulphur – is stored in organic matter and only becomes available as organic matter breaks down.

Other nutrients

Trace elements such as copper (Cu), zinc (Zn), manganese (Mn), iron (Fe) and boron (B) are only required in small amounts. Soil testing only provides a guide to the levels in the soil and can help identify gross deficiencies or toxic levels. Tissue testing provides a more accurate measure of trace element imbalances.

Soil acidity (pH) and aluminium (Al)

Soil acidity and alkalinity are measured as pH. There are two methods to measure pH – one is in calcium chloride (CaCl2) and the other is in water (H2O). The water measure is the traditional method but results can vary throughout the season.

Aluminium is stored in the soil in a number of forms that can be toxic to some plants. The level of toxic aluminium is affected by pH. As pH decreases (soils become more acid), more aluminium is converted to the toxic form.

Figure 6.3 In a lot of acid soils, lime is a necessary input to ensure maintain a healthy growing environment.
Source: NSW DPI

Salinity

Salinity is measured using electrical conductivity (EC) by passing a current between a water extract from the soil sample. As salt conducts electricity, the more total soluble salt (TSS), the higher the reading, which is recorded in deci-siemens per centimetre (dS/cm).

Soil structure

Poor soil structure affects root growth and water infiltration. The stability and structure of soil depends on soil organic matter, the levels of calcium (Ca), which hold soils together, and elements which disperse soil, such as magnesium (Mg) and sodium (Na).

Sodicity refers to a soil property where a significant proportion of sodium exists in the soil compared with other cations on the exchange complex. A soil is considered sodic when there is sufficient sodium to interfere with its structural stability, often affecting plant growth. Sodic soils tend to suffer from poor soil structure, including hard-set soils, hardpans, surface crusting and rain pooling on the surface, which can cause problems for erosion, water holding capacity, water infiltration, drainage, water run-off, plant growth, cultivation and access to paddock with machinery.

Useful soil test results include the ratio of calcium to magnesium (Ca:Mg) and the total amount of sodium compared with other elements (called the Exchangeable Sodium Percentage or ESP).

Additional indicators

A number of other figures and calculations are provided in soil tests which are used to calculate the rate and type of product to apply.

These include the following:

  • Phosphorous Buffering Index (PBI): a guide to the amount of phosphorous applied to a pasture or crop that is ‘locked up’ on soil’s clay particles and is not available for plant growth.
  • Cation Exchange Capacity (CEC): cations are soil components that trap and release nutrients to the soil water.
  • Soil texture: a measure of the proportion of sand, silt and clay in the soil. It influences the availability of some nutrients, a plant’s reaction to salinity and the requirement of soils for products such as lime and gypsum.
  • Organic carbon: levels of organic carbon influence soil structure and CEC. The breakdown of organic carbon is critical to the release of other nutrients.

Take soil samples for testing and interpret the results

Tool 6.6 provides the directions for taking a soil sample for analysis at an accredited laboratory.

While soil tests can help identify which soil factor or factors are limiting production, the target application of various products will depend on the soil type, rainfall, pasture species grown and the stocking rates.

Consult your local agronomist or product reseller to assist you in identifying which deficiency is limiting production and calculating the quantity of particular products to apply in terms of nutrients, lime or gypsum. They can also look at the products available and calculate which one is the most cost‑effective to apply.

Interpreting soil tests as part of developing a fertiliser strategy is discussed in Tool 7.3 in MMFS Module 7 Grow More Pasture which considers the use of phosphorus, potassium, sulphur and nitrogen.

Tool 6.5 is provided to help interpret soil tests for any soil health problems (acidity, sodicity, salinity and trace elements) on your farm.

Visual indicators of soil condition

Visual indicators of soil condition can be useful to help diagnose underlying soil constraints, especially in the absence of soil test results. These indicators include general pasture appearance, individual plant symptoms, the type of plants and weeds which grow as well as appearance of the soil itself.

The best time to look for plant indicators of nutrient deficiencies are late winter and early spring. At this time, potassium, nitrogen, and sulphur may have been used up or lost due to wet conditions and nutrient demand by plants is increasing. Fertility indicators include:

  • Urine or dung patches: Dark green patches with greater growth of grass or clover, paler green in other areas or increased or fast pasture growth surrounding manure pats, shorter paler green growth elsewhere.

Pale green areas indicate pasture may be deficient in potassium, nitrogen, or sulphur. Urine contains high amounts of nitrogen and potassium and some sulphur. Dung affected areas also contain phosphorus. Or it could indicate selective grazing as stock avoid pasture near dung while odour remains (up to three months).

Figure 6.4 Dark green patches responding to urine and dung.
Source: MLA

Yellowing or pale green colour: indicates deficiency in potassium, nitrogen or sulphur or trace elements or possibly waterlogging, resulting in transient nitrogen loss.

 

Figure 6.5 Transient nitrogen loss leading to yellowing.
Source: MLA

  • Grass-dominant pasture with little or no legume and slow growth: possible phosphorus or molybdenum deficiency, or low soil pH (soil acidity), or possibly inappropriate sub clover management.

 

Figure 6.6 Grass-dominant pasture because of poor sub clover management.

Source: MLA

  • Increased growth and high fertility indicator weeds growing on stock camps: indicates high soil fertility – stock empty out dung and urine, so nutrients become concentrated. A useful fertility diagnostic tip is to pick a desirable grass tiller or clover leaves from stock camps/urine patches and compare leaf sizes to the rest of paddock.

 

Figure 6.7 Stinging nettles growing in abundance under this tree which is commonly used as a stock camp.

Source: MLA

  • Areas that stay green during summer but have reduced growth: indicates salinity caused by a salty water table less than two metres from the soil surface or a freshwater spring. Bare patches remain damp and white salt crystals may be visible on soil surface. Different plant species grow compared to the rest of the paddock. Observed late spring.

 

Figure 6.8 Salt-affected areas which remain damp often grow different plant species compared to the rest of the paddock.

Source: MLA

Lucerne stunting or patchy poor growth following establishment: observed in the first three- to four-months after establishment indicates soil acidity with associated high soil aluminium. This affects root growth, causing stunting, sideways growth of roots and plant loss. Waterlogging may cause a similar effect.

 

Figure 6.9 Soil acidity, and associated high soil aluminium levels, and waterlogging affect lucerne root growth, causing stunting, sideways growth and plant loss.

Source: Malcom McCaskill, Agriculture Victoria

High content of the following weed species indicate high fertility:

  • capeweed (Arctotheca calendula),
  • barley grass (Hordeum leporinum),
  • marshmallow (Malva parviflora) and/or thistles within pasture or in stock camps, gateways or adjacent to tree plantations.
  • High fertility, particularly nitrogen. Presence of barley grass also indicates high phosphorus levels. It can also indicate overgrazing in late summer which provides ideal conditions for germination.

 

Figure 6.10 The presence of capeweed (Arctotheca calendula) often indicates high fertility, particularly nitrogen.

Source: MLA

High content of the following weed species indicate low fertility:

  • Flatweed (Hypochaeris radicata) and/or sweet vernal grass (Anthoxanthum odoratum) – low potassium. Common on light textured soils (as potassium leaches) and on paddocks repeatedly cut for hay or silage.
  • Bent grass (Agrostis species) and/or fog grass (Holcus lanatus) – low fertility, especially nitrogen but also phosphorus, potassium and sulphur or soil acidity.
  • Silver grass (Vulpia bromoides) – low nitrogen or soil acidity.
  • Onion Grass (Romulea rosea) – low phosphorus.

 

Figure 6.11 A lot of flatweed (Hypochaeris radicata) can indicate low potassium levels.

Source: MLA

Slow and poor growth of pasture occurs from ‘hidden hunger’ of nutrients before the appearance of leaf symptoms. Individual leaf symptom indicators can occur when deficiencies are extreme include:

Small, stunted, or dark green leaves on sub clover plants: observed in early spring when clover is adequately growing and indicates possible phosphorus deficiency. Sub clover leaves with adequate fertility should be the size of a 20-cent piece.

Figure 6.12 Sub clover leaves with adequate fertility should be the size of a 20-cent piece.

Source: MLA

Bronzing of sub clover leaf margins which develop into pale grey spots: observed in late winter to early spring. Indicates potential potassium deficiency.

Figure 6.13 Bronzing leaf margins which develop into pale grey spots can indicate potassium deficiency.

Source: James Easton, CSBP

Stunted sub-clover plants, usually pale green in colour: observed in autumn and winter, indicates soil acidity and associated high soil aluminium, or the presence of soil borne diseases – likely caused by four main pathogens (Phytophthora, Pythium, Aphanomyces, Rhizoctonia) – which cause root pruning and brown lesions on roots.

Figure 6.14 Stunted sub-clover plants, usually pale green in colour, indicates soil acidity and associated high soil aluminium, or the presence of soil borne diseases.

Source: Sue Briggs, CSBP

Few or whitish nodules on legume roots: observed 12 weeks post-germination and indicates inadequate nodulation. There could be many reasons for this, including soil acidity and high soil aluminium, insufficient rhizobia in the soil as a result of cropping for many years, residual herbicide damage, molybdenum, or sulphur deficiency.

Figure 6.15 Inadequate nodulation can occur for many reasons and will require further investigation.

Source: Jo Powell, NSW LLS

Tool 6.6 explains how to do these tests. For more information on interpreting soil test information see signposts.

Predicta B

PREDICTA® B is a rapid diagnostic test to identify soil borne diseases (such as Pythium, Phytophthora, Aphanomyces and Rhizoctonia) which cause root rot and damping off, particularly in legumes.

Testing has traditionally occurred in the cropping phase as the testing procedures are more advanced in cereals. However, it is now possible to test pastures to detect high, medium and low population densities of these major soil-borne diseases.

PREDICTA® B testing is conducted by South Australian Research and Development Institute (SARDI). Contact SARDI to discuss test options and locate accredited agronomists who can take samples.

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