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Soil Organic Matter
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  1. Default Soil Organic Matter

    A useful post from the defunct Rural Network forum, by Dr Doug Edmeades.

    Soil organic matter – what is it and where does it come from?

    The importance of soil organic matter, or to use the colloquial term, humus, has been known for centuries – certainly long before the Organic Movement. Most text books will list the benefits of soil organic matter (relative to soil with little or none of it) as improved soil structure, water holding capacity, storage of nutrients and better heat absorption. Soil organic matter is also the home and food for the myriad of soil micro and macro organisms from earthworms and insects to bacteria, fungi and the tiniest protozoa.

    We are blessed in New Zealand because our well developed pastoral soils, taken in the international context, contain large amounts of organic matter. This is a consequence of our temperate climate, and our clover-based, grazed pastoral system.

    Soil organic matter (SOM) - humus - comprises the breakdown products of plant and animal (dung) material returned to the soil. The fresh plant material and dung returned to the soil is food (energy) for soil bugs which get to work in a sort of chain gang and break this material into increasingly smaller and more stable units, which are then often joined together (polymerised) into stable, large, complex organic substances. Humus is dark coloured and as a general rule the darker the colour and the deeper it extends into the topsoil the better the soil. It is this colour that enhances heat absorption.

    In our grazed, clover-based pasture, carbon (the major component of soil organic matter) comes into the system from the atmosphere (as carbon dioxide) via the plant (photosynthesis), some of which goes into the soil as plant residues (from tops and roots) and some via the dung. The amount of carbon added from these sources is of the order of 1-3 tonnes per hectare per year annually. Losses occur from the animal because it breaths out carbon dioxide (respiration) and belches methane, and from the soil via the oxidation of organic matter.

    The key point is this: if the sum of the inputs is greater than the sum of the outputs then carbon and hence organic matter is accumulating in the soil.

    So, how should we manage our soils to ensure that this happens or that at least we are not depleting soil organic matter levels and hence jeopardizing soil quality and contributing to green-house gas emissions?

    Soil organic matter – how should we manage it?

    Several studies in the 1950s and ’60s showed that soil organic matter accumulated (inputs are greater than outputs) following pasture improvement (i.e. clover + fertiliser + animal). This accumulation continues for about 20-50 years and then reaches a steady state (inputs = outputs). The time required to reach this steady state, and the amount of soil organic matter present at steady state depended on the climate and the soil group. Generally, the wetter and warmer the environment the more soil organic matter.

    Thus the management recipe was simple: clover (to add nitrogen), fertiliser (especially phosphorus, potassium and sulphur - PKS - to maximise clover growth), and the animal (to do the recycling) plus time equals more soil organic matter.

    The situation under cropping is very different. Cropping exploits soil organic matter (outputs are greater than inputs) and this is especially so when the crop residues are removed. So the second management lesson in terms of soil organic matter management is: do not crop if you can help it! Or if you need to crop make sure there is a good rotation from clover-based, grazed pasture to crop and then back again. Green manuring or heaps of compost are also helpful. Civilisations have failed by not following this simple rule.

    A number of more recent studies suggest we need to modify slightly our understanding of soil organic matter accumulation.

    Tate (1997) compared the soil organic matter contents of 43 topsoils sampled first in the 1960s and again in 1992. He concluded that there was no change over this period. This is consistent with the idea that the soils were at a steady state with respect to soil organic matter accumulation, as discussed above. In contrast, Schipper et al (2007) reported an average decline (about 1% or 1 tonne SOM/ha) in 37 sites over a period of about 20 years.

    How do we reconcile these studies – one suggesting no change the other indicating a small decline?

    Other researchers have dug deeper into this apparent paradox and have reported results which indicate that soil organic matter can be reduced by:

    Land-use intensification – management practices which increase pasture utilisation (e.g. better grazing management, increasing stocking rate, introducing irrigation) and hence reduce the proportion of plant material (litter) being returned to the soil and thus result in the steady state soil organic matter being reduced.

    Changes in the quality of the litter returned to the soil – it is suggested that some of our newer management practices (and this includes all those listed above plus the introduction of new pasture cultivars and the introduction of fertiliser N) result in a change in the chemical composition of the litter returning to the soil allowing it to be more readily broken down in the soil and hence less is conserved in the soil organic matter pool.

    Two points must be emphasised: First, even if the figures reported by Schipper are true, (i.e. a decrease in SOM at the rate of 1% per annum) there is no need for panic or alarm. As stated earlier, our developed pastoral soils already contain large amounts of soil organic matter.

    Pastoral agriculture in New Zealand is not on the verge of collapse. I stress this point because of our propensity in this PC and environmentally sensitive age, to seize on and highlight the negatives, especially on environmental issues. Second, in the scientific sense, the possibility that modern management practices are depleting soil organic matter levels is somewhat speculative. It is an emerging issue and more science is most definitely required.

    The above is a summary of a talk I presented to a special meeting of the NZIPIM. It is also the origin of a formal paper presented to the FLRC Conference (see Metherell, Edmeades and Ghani 2008, Massey University, Fertiliser and Lime Research Centre Workshop, February 2008) and an adaptation was published in the Fertiliser Review No 20.

    Dr Doug Edmeades is a soil scientist of independent fertiliser consultancy AgKnowledge www.agknowledge.co.nz/

  2. Default

    Doug, I take your point that more research is needed in this area. Is it possible that Tate(1997) saw no change in soil carbon levels yet they might have improved and declined again during that 30 years?

    There is a great variation in the depth and quality of topsoils seen around the Waikato. Are all of these soils at their steady (best) state?

    It would be very disappointing to give up on the idea of continually improving the soil and profitability on the land you own. And what a great story if we can show that net carbon is being continually sequestered in that very large mass that is NZ topsoils. Most of NZ is covered in grass, and the average energy conversion efficiency to grass sugars in NZ from the sun is just 2%. It’s nearly as low through ruminants, resulting in an average energy conversion from the sun’s total blackbody radiation/Ha to say milksolids energy from each hectare per year, of 0.06%.

    Is that the best we can do? On the average pugged or damaged pasture there might only be 50% green showing to the sun, the rest is dirt.

    Recent concentration on kgDM/Ha/yr could be a recipe for growing bulk poor quality grass at the expense of the soil, the environment and the bottom line.

  3. Default

    Dr Edmeades replied (excerpts):

    I think it is unlikely that soil carbon levels (as in the Tate study) would fluctuate in that manner. They (soil carbon levels) are normally quite stable and do not change either up or down very quickly.

    Are all Waikato soils at steady state? I think this is more likely than not but the only way to be certain in a given farm situation is to measure soil carbon levels over time and this would need to be done for long periods of time (decades) to pick up any trend. Also it would need to be measured down the soil profile.

    Yes, there has been until recently a focus on DM/ha for the simple and sufficient reason that our past science was saying more DM in more milk or produce out. This has now become more refined and now there is emphasis on the components of DM (fibre, carbohydrates etc). This is not a change in science direction - it is simply science becoming more specific and refinined.

    It would be nice to think, as you suggest, that soil carbon would continue to accumulate over time and hence become a never-ending sink for carbon - but sorry -I did not design the system. In any case do we all want to farm peat soils?

    Doug Edmeades | May 21, 2008 |
    Last edited by Graham; 13th August 2009 at 12:53 AM.

  4. Default

    Let's say we wanted to offset the entire country's greenhouse emissions by storing carbon in pastoral soils.. how practical would that be?

    NZ has about 39% of its land in pasture, or 10,538,500 Ha of grassland, most of it higher-producing exotic grasses. Our total emissions (agriculture, transport etc) are 75,500Gg of CO2-e per year, or 75,500,000 tonnes of CO2 equivalent.

    So we'd need to store 7.2 tonne of CO2-e per hectare, per year. That's 720grams per square meter. Grasses grow about 20 tonne of drymatter per hectare per year at best in NZ, which is 2000 grams DM per square meter. (The grass raw energy conversion efficiency is quite low at about 2%.)

    Since profitable pastoral farming relies on stock eating most of the grass produced, the sequestered amount of carbon needed, looks a bit too high. But ruminants only use up about 10-65% of the organic matter they digest, and excrete the rest.

    Of course, the soil organic matter is continually being consumed by soil organisms, and grass is one of the fastest materials to be used up in this way. Wood and bark takes a lot longer. And I'm not sure what mass of soil organic carbon is equivalent to a gram of CO2-e.

    However, everyone is in agreement: more soil organic matter (SOM) is a good thing in general. It holds more moisture in the soil, and retains minerals and elements ready for plant use, by encouraging biological life in the soil. SOM also brings with it, many of the nutrients needed by plants. More SOM allows soil to breathe, and generally attain a crumbly texture.

    The pastoral system relies mainly on leaf litter and dung/urine to be returned to the soil. Using fertilisers increases grass growth (NPK plus trace elements) and this helps the cycle. Using legumes to fix nitrogen is a preferred option.

    Many of the exotic grasses used here in NZ, have shallow roots in normal situations, and growth tends to drop off markedly in drought conditions. As a lot of soil carbon is built up from decomposing and shedded plant roots, it would make sense for these roots to be as bulky as possible for most of the year.

    While not a common practice here, yeoman ploughs will cut vertical slots in the soil and trim the lower part of grass roots off horizontally. This aerates the soil and breaks up any hardpan structure, doesn't lose a lot of SOM, and accelerates the production of more SOM from the dead roots. Presumably this work is done when moisture levels are good, and the grasses soon grow back down into the soil. Some startling reports (not peer reviewed) about increases of several inches of topsoil/SOM in just a few years are made.

    Since it is known that pasture soils can take many decades to reach equilibrium in terms of SOM, it just takes some new farming practices to perhaps set up a new higher equilibrium, and our farmers could then claim carbon credits for farming in this way. All the while their productivity should be increasing as well.

  5. Default

    Local farm consultancy business, eCogent in Cambridge, has been a champion in using Brix pasture and forage measurements as a farming benchmark. Headed by Peter Floyd, over 200 farms are using their system, which uses several "truths" including Brix measurements. Their approach so far has been to compare two similar forages, and feed the animals the highest Brix on a given day. Rather than quote lab results, their emphasis is on rising farm profits as the ultimate result.

    Biological farming techniques are high on their list too. Today, the Waikato Times reported that eCogent customers who "benchmarked soil carbon levels last spring, using protocols designed by Landcare Research scientist Graham Shepherd, had [soil carbon] increases from 5% to 10%, representing up to 10 tonnes of carbon per hectare".
    Peter is quoted as saying "The highest figures are extraordinary".

    Yes Peter, they are! This is right in the required range I calculated above. Based on this work, it should be perfectly feasible for NZ's pastoral farmers to completely cancel out all of the entire country's emissions! And make a lot more profit in the process. These findings deserve immediate testing and confirmation by the scientific community.

    I'm sure Peter would be happy to see them peer-review it to death..we should be so lucky. This basic work should have been done a long time ago, but I think it has been bypassed in favour of chemical fertilisers, treatments, special grass breeds, etc etc. I don't think any pastoral scientists even know how to use a Brix meter. My contention is that a Brix meter gives a very good indication of soil biological activity when used carefully, and on a trending basis. A lot easier than counting worms etc.

    Of course, setting soils up with lime and other additives is the important starting point, and this does take 2-3 years or more.

  6. Default

    I think Peter is way ahead of us on this point - he has already linked up with his old university, Massey, and his results are probably a big part of the reason Massey is heading down the biological farming path, recently announced.

    What will be your legacy? – Peter Floyd - Rural News 28 September 09

    It has been an amazing couple of weeks. Two very special events for me, and in a strange way they are linked.

    The birth of our first grandchild, Baxter, was indescribably wonderful, and I would never have believed what a difference such an occasion could make to our lives. Those of you who are grandparents will understand, I am sure, how overwhelmed Gillian and I have really been by the experience. Yes, mother and son are both well and facing the big wide world with plenty of vigour and determination.

    The second significant event was the partnering up of eCOGENT Farm Business Systems with Massey University's commercial arm, the Auckland based e-centre. This is an important step which will help us grow the business and make more New Zealand pastoral farms increasingly profitable and more environmentally sustainable.

    The partnership comes on the back of just-completed Massey University research showing that the majority of our members are seeing a clear improvement in farm profitability. Commissioned by Investment New Zealand, the independent survey also shows eCOGENT farms have reduced their environmental impact through less intensive stocking and through a reduction of over 60% in their use of nitrogen fertilisers. This was achieved against a backdrop of improvements to soil, pasture and animal health.

    By coincidence it is almost exactly 50 years to the week since I completed my studies at what was then Massey College. When I think back to those early learning days at Massey and reflect on the soil and pasture management lectures we were given, I can see how far current farm practice has moved away from those basic principles in the quest for more production.

    My memory of farming back then is one of abundant supplies of multi-species pasture, normally a night paddock and two day paddocks and the odd stack of hay. They were days of healthy animals, healthy and happy, low stressed people who had bank balances usually in the black.

    I think of all of the fashions that have been introduced since that time under the guise of improved management for more production, and the confusion and frustration they have caused and the incredibly high farming costs that farmers have had to bear as a result.

    And what is the legacy of this never-ending quest for greater and greater production? Depleted soils, monoculture pastures, sick stock, high animal health bills, high debt, high blood pressure, dirty streams, contaminated groundwater, loss of microbiology, increased emissions of nitrogen gases, and a reputation for farming as a “cost” to the country because of environmental damage.

    The lesson I have learnt over five decades since those Massey College days is that it just doesn’t have to be that way. We now have a structured, sustainable approach to farm business that hauls eCOGENT farmers back from the brink, removes much of the guesswork and risk from management decisions, and allows them to take control of their environmental and financial performance.

    A critical tool for doing this is financial software that forecasts the daily profit from the dry matter consumed by each class of livestock. This results in more objective and more profitable stocking and farm management decisions. This approach plus the link with Massey University e-centre gives me new hope that pastoral farmers will be able to achieve sustained environmental improvement, sustainable profits and a valuable asset to pass on to their children’s children.

    These goals have always been important to me but the recent new arrival has given them new significance. Both the eCOGENT Process and a better environment are part of the legacy I want to be able to pass on to the precious newest member of my family.

    Peter Floyd is the Managing Director of eCOGENT
    www.eCOGENT.biz ph 0800 433 276

  7. #7

    Default Organic Matter

    Hi Graham,
    Just a few notes on humus.
    The organic matter reading on a soil test should be divided by 1.7 to get an organic carbon equivalent.
    Organic matter, as measured on most soil tests, is actually a combination of three different materials:
    1) Raw organic matter
    2) Active Humus
    3) Stable Humus

    Stable humus is the important part!
    Benefits of Humus
    Drought Resistance - Holds 80% to 90% of its weight in water. Microbes, which live in stable humus, emit a gum-like mucilage, which also helps to retain moisture in the root-zone.
    pH Buffering - pH extremes have a profound effect on nutrient availability. Humus can neutralise the negatives associated with these extremes.
    Mineral Retention - Humus has a Cation Exchange Capacity (CEC) of 250 and can complex minerals to prevent them from leaching.
    Crumb structure - the sticky exudates secreted by microbes in the process of forming humus, ‘glue’, soil particles together to create a highly desirable crumb structure.
    Soil Detoxification - Heavy metals and chemical residues can be isolated and immobilised to reduce damage to both plants and micro-organisms.
    Root-Zone Chelation - The humic and Fulvic acid component in humus chelates minerals to enhance mineral uptake.
    Plant Growth Stimulation - Humus is a storage system for all of the beneficial microbial exudates, including enzymes, vitamins, hormones and antibiotics.
    Solubilization of Mineral Fertilisers - Materials like rock phosphate, lime, gypsum and rock dust are solubilized far more rapidly when humus levels are good.
    Sodium Management - Humus buffers the damage to plants and micro-organisms associated with high-salt fertilisers or saline irrigation water.

    Brett Petersen

  8. Default How NZ could lead the World?

    Thanks Brett. I see what you mean, SOM is a good thing to have. If soils lose it, they tend to compact, don't drain well, poor aeration, plant roots are stunted etc. Sounds familiar.

    I've had a bit of a look on google for now, and identified that your figure of 1.7 relates to the carbon content C of SOM being around 1/1.7 by weight, or 58%. In turn, SOM is generally 2% to 5% of the total weight in the top layer of a soil (about 35cm deep). If soil is treated as that deep, then one Ha of topsoil weighs about 4700 tonne, and most scientists give a figure for the Waikato soil of 100 tonne of SOM/Ha, just over 2% by weight. By definition SOM can include living biological matter as well as humus etc.

    Now this next bit might be very wrong, as it's sourced from a dubious blog site (unlike this one of course!). If all of that SOM carbon is sourced from CO2 in the air, and carbon is just a part of that CO2 molecule (12/12+16+16) = 27.3% by weight, then one tonne of carbon held as SOM, uses up 3.67 tonne of CO2-e!

    My previous post showed that to cancel out all NZ's GHG annual emissions with grassland soils, we'd need to additionally store about 7.2 tonne CO2-e per hectare, per year. This is starting to look achievable, as it is only about 2 tonne of soil carbon, or 3.4 tonne of additional SOM per hectare per year.

    OK, that's a 3.4% increase in SOM per year for now, but over time it will be a reduced percentage, the same mass needed. On a per square meter basis, we currently have 10kg of SOM per m2 of soil on average, and we need to sequester another 340g each year. It doesn't seem impossible.

  9. Default Not so easy

    Since I last posted, I spoke on the phone to Assoc. Prof. Louis Schipper at the University of Waikato about measuring carbon in soils. I didn't make good notes at the time, but the gist of the conversation was this:

    There was some dismay on his part about the known claims from Peter Floyd at eCogent regarding up to 10tonne/Ha extra carbon being stored on farms under their system.

    His explanation of this was clear. It's a very expensive process to pyrolise soil from carefully selected sites, so that the 'before and after' carbon readings can be accurately ascertained. But as you are starting with about 100tonne/Ha anyway, measuring a 10% increase for example, would need to be very accurate. This pyrolising process is an accurate system, where the soil is burnt off and the energy released from the carbon is measured.

    If a qualitative measurement by visual assessment (Shepherd, Landcare) is taken, which has an error of just (say)+/-8% at the start, and another of +/-8% a year or two later, the total error is +/- 16%. That's basic NCEA level one maths, or School Certificate level. So a figure of 10% increase in carbon would have to be bracketed by the error in that measurement, in this case about +/- 16 tonne carbon/Ha. The error might well be a lot more.

    Peter needs to send at least some of these soil samples away for expensive lab testing, so that the qualitative technique can be benchmarked. These results should then be published somewhere for all to see.

  10. Default

    I have been thinking that many farms might benefit from a tilling system that introduced compost into poorer soils, while breaking up the hardpan. I guess that would be expensive to operate. But this item from Ruralnews shows the result on crops..

    Compost builds yield but what cost?
    by Andrew Swallow

    Compost’s interaction with conventional fertiliser is being investigated as part of the Lincoln trial, explains Plant and Food’s Craig Tregurtha.Crop yields can be substantially improved by hefty applications of compost, a FAR organised field day near Lincoln was told recently.

    However, limited supply, variable response and substantial delivery and application costs means it will need to be carefully targeted to be economic.

    Trials in South Canterbury have already shown the yield enhancing potential of the product, 50t/ha applied prior to sowing boosting kale drymatter yield 50%, from 8t/ha to nearly 12t/ha, with a 25% benefit to the following year’s kale, though barley this summer, the third since application, didn’t respond.

    “It looks like there’s very little in it in terms of grain yield though we did see height differences in the barley,” says Plant and Food Research’s Craig Tregurtha.

    That South Canterbury work is ongoing with oats/moata already sown for winter grazing, to be followed by kale and possibly barley again after that, but a new, more in-depth trial with a more typical cropping soil and rotation has been established at Lincoln.

    Following 0, 25t and 50t/ha applications of compost to deep, paparua silt loam on Plant and Food’s farm, forage maize was sown, to be followed by wheat this autumn, oats/moata for winter 2011 and a crop of peas or barley in 2011-12.

    Compost has either been applied in one hit, incorporated into the Lincoln soil (it was broadcast pre direct drilling in South Canterbury) or will be split applied across the three phases of the rotation. Overlaying those plots are four nitrogen rates.

    “We’ve tried to make it a fairly typical arable rotation but also to make best use of the trial opportunity,” says Tregurtha.

    A recent history of intensive cropping and cultivation means the Lincoln soil is low fertility and structure is “shot”, notes Tregurtha’s Plant and Food colleague Shane Maley.

    “The soil’s pretty much like flour.”

    How compost changes that will be monitored, as will moisture retention and distribution of nutrients through the soil profile to 1.5m deep, something that is impossible on the South Canterbury site due to stony subsoil.

    Tregurtha says poor structure as seen at Lincoln is not unusual: “Across the Canterbury Plains there are a lot of paddocks like this that could really benefit from the use of composts.”

    However, as various speakers at the field day noted, the challenge is to get compost from processing sites near large towns such as Christchurch and Timaru, which supplied the Lincoln and South Canterbury trials respectively, applied on farm in sufficient volume to make a difference without blowing the budget.

    Transpacific Industries, which runs the Timaru District Council composting site and is a 50:50 partner with Living Earth in Christchurch’s composting facility, says it is charging $30/t for its product ex-depot, with about 13t normally fitting in truck.

    “We’re still doing work to get a realistic price based on its value, but we’ve got to be prepared to meet the market. The bug bear is it is so bulky,” says Transpacific’s organic processing planner Geoff Hemm.

    For $30 buyers get $65-$70-worth of nutrient, but have to a pay a premium for spreading, he acknowledges.

    Timaru’s green waste is being turned into about 8000t/year of clean, screened, weed-free compost by Transpacific while Christchurch generates about 70,000t though the potential is 100,000-120,000t says Living Earth’s George Fietje.

    The Lincoln trial is funded by MAF Sustainable Farming Fund with composter Transpacific Industries, Canterbury Waste Joint Committee, Environment Canterbury, FAR and Ballance Agri-Nutrients.

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