Showing posts with label phosphorus. Show all posts
Showing posts with label phosphorus. Show all posts

Tuesday, December 16, 2008

Fertilizer prices suddenly collapse in late 2008

The International Center for Soil Fertility (IFDC) reports that, with the exception of potash, world fertilizer prices have dropped dramatically.


Gregory explains why fertilizer prices fell so rapidly in late 2008. "The high fertilizer prices caused 'demand destruction.' Farmers were unable or unwilling to pay two or three times the prices of early 2007." Collapse of the global credit market, a trade recession, and slowdown in world economic growth worsened the situation. Demand for fertilizers fell and stocks accumulated. Fertilizer manufacturers cut back on production.

"But potash prices have stayed high due to its shortage and difficulties in transporting Russian potash because of an enormous and expanding sinkhole near the Silvinit mines," Gregory says. "Demand for potash increased from 2006 through 2008, and potash inventories are now 37% lower than over the past 5 years."

A couple of thoughts I will be researching.

First, if lower demand has translated to lower utilization, this should show up as reduced inventories of 2008 commodity crops, like rice, soybeans, and wheat, and reduced supply of perishable fruit crops like bananas.

Second, with fertilizer prices now low, this would be a excellent time to replenish African soil fertility, currently in crisis. Especially in consideration of a possible reduction in 2009 food inventories world wide.

(recycled from nscss.org)

Monday, June 09, 2008

No Miracles

Charcoal cannot replace the need for adding mineral nutrients.

I am an unabashed charcoal enthusiast. Used properly, adding charcoal to soil improves biomass production and soil health. Sometimes dramatically when soil productivity is low. Certainly part of the effect is increased nitrogen use efficiency: less N lost to nitrification and leaching. Charcoal also tends to be associated with higher post harvest soil levels of P and K for reasons that are not entirely clear. Perhaps this effect also is due to increased efficiency.

Most TP enthusiasts, myself included, are convinced that the most mysterious effects from adding charcoal relate to soil biology, more than they relate to direct physical and chemical effects, although those realms play important roles also. And, in keeping with my previous post, it seems clear to me that increased energy efficiency is a critical bit here. Plants and microbes are growing more biomass with less effort for reasons that can't be entirely explained by traditional nutrient-based perspectives. Yes, the charcoal adds potassium, yes it raises soil pH, yes it increases soil water and nutrient holding capacity. But the results speak to more, much more.

The behavior of charcoal amended soil seems to defy the limits of the soil-biology system understood by traditional science. However, it would be entirely foolish to think that simple soil nutritional requirements are not still in play. Nutrient deficiencies limit living systems. Charcoal may promote efficiencies that help stretch the budget in regards to those limits, but in the end, the most limiting nutrient before adding charcoal is probably still going to be the most limiting nutrient after adding charcoal.

What got me thinking about this was consulting soil scientist Doug Edmeades’ posts on soil organic matter. The first, Carbon farming: take-off or rip-off, explored how carbon sequestration efforts can cut both ways. The second, Soil Organic Matter Matters, hits on the most-limiting-nutrient.

Pasture plants need 16 nutrients. Without all 16 the clover will disappear, the pasture will be N deficient, the quality grasses will fail, pasture production would collapse followed by a need to cut back the stocking rate and, given sufficient years, a farm would be back to native pastures and bush. In the process soil carbon levels would decline.

Collapsed pasture production is no idle threat. We know that the collapse of legumes in pasture systems in Europe and in the eastern US helped motivate the expansion of the western US. Against that historical backdrop, Benjamin Franklin famously demonstrated sulfur deficiency when he added gypsum to alfalfa to form the words "This has been plastered". Doug Edmeades mentions this because soil carbon sequestration enthusiasts seem to have temporarily lost track of these limits. The same caution applies to charcoal.

There is great potential for increasing productivity through judicious use of charcoal. However, TP enthusiasts must not lose sight of the fact that charcoal cannot replace the need for adding mineral nutrients.

Saturday, February 24, 2007

Home Grown Biofertilizer


The role that soil microbes (archaea, bacteria, and fungi) play in soil nutrient availability is an interesting area, one where we have much to explore. Biofertilizers are increasingly available commercially, meaning those of us outside the academic community will have increasing opportunity to conduct our own reseach. From Montana State University:

Some soil bacteria and fungi can access otherwise unavailable phosphorus, and some are commercially available. In a study on barley, one of these bacteria increased phosphorus availability by about 10 percent. In another study, a phosphate-solubilizing fungus was found to increase spring wheat grain yield by nine percent. "For both studies, the economics need to be considered to determine if these increases are worthwhile, and additional research is needed to determine the effectiveness of these products for different crops and soils," Jones said.


Growing your own biofertilizer may not be that difficult, depending on what it is you are trying to grow. Pictured is some compost tea starter I am "growing" for tomorrow's 36 hour run of actively aerated compost tea. I am going for a fungi-rich tea. Since the aerated tea process favors population growth of bacteria (and, one would think, archaea) over fungi, I am giving the fungi a boost before I start the tea. To 2 cups of compost, I have mixed in 3 tbs oat bran (the white flecks) and 1 tsp of T and J Enterprises (Spokane, WA)'s trichoderma rich "Soil Life & Activator" mix. As you can see the fungi is doing mighty fine. My first couple runs at promoting fungi growth were not as successful. By the looks of this one I am starting to get the hang of it.

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Saturday, December 09, 2006

Soil and Bioavailability of P in Food


Researchers find that soil phosphorus levels may affect plant phytate levels as much as plant breeding. Phytate is the principal storage form of phosphorus in many plant tissues, especially bran and seeds.

Phytate is generally not bioavailable to humans and non-ruminant animals. Accordingly, there has been a push to develop low-phytate crop varieties. Not only is the phosphorus in low-phytate grain crops more digestible by people, low-phytate grains free up minerals essential to human nutrition: zinc, manganese and iron. This new research shows that grain raised with higher levels of soil phosphorus can have higher levels of phytate. I have not read ($) the journal article, but my thoughts are that the discovery of this soil connection was not anticipated: normally nutritional availability does not decrease with increased soil nutrient levels. If this relationship can be validated, it is an important breakthrough that affects human nutrition, efficient use of phosphorus (a non-renewable resource), farm costs, and environmental quality.

Swine and poultry operations benefit. Low-phytate feed results in lower manure phosphorus for these non-ruminants, a welcome prospect for waste management and addressing water quality concerns. Swine rations often need phosphorus added to ensure bone and muscle development for rapid growth, driving the market development for new, low-phytate crop varieties. The alternative to low-phytate feed is to use a feed additive, phytase. Currently, neither approach is particularly cheap.

Appreciation and attribution:
Sugar Creek Farm for a great photo.
GMO Pundit aka David Tribe for posting on this.

($) According to my read of HighWire Publishers Free Online Full-text Articles list, the journal article will be made available at no cost April 2, 2008 (18 months after publication).

Tuesday, December 27, 2005

Phosphorus and TMDL

Today I am pulling together conceptual information related to phosphorus (P) and Total Maximum Daily Load (TMDL) in anticipation of meeting with Walt Edelen and Rick Noll, water quality folks with the Spokane County Conservation District (SCCD). The problem we will be putting our heads together on is the relationship between river and stream P levels (ug/l) relevant to TMDL and soil P levels (mg/kg) in adjacent, contributing areas. More specifically, we are going to lay out what methods and approaches are available for gathering soil P information that will produce data that can be used to measure P loading, measured in pounds of phosphorus, lost to the river. We want tools to quantify the effects of implementing various Best Management Practices (BMPs) for controlling streambank sluffing and farm field erosion.

The motivation for specifically defining pounds of phosphorus delivered has to do with the concept of phosphorus load allocation. It has to be conceptual, rather than actual, because, when it comes to soil contributions, we don't have the studies needed to characterize the complex causes and effects in these systems. Nor do we have the luxury of time of waiting for the studies to be designed, funded and conducted. The TMDL beast is at the door.

At first glance, it seems like a simple question of mass balance. How many tons of soil are discharged to the river, where and when, and how much phosphorus did it have in it. A mass balance approach certainly makes sense for wastewater dischargers, considered the most significant source of P in the Spokane river. But that approach doesn't fit as easily for soil. How much soil phosphorus converts to water phosphorus. It can't be 100% efficient, some will end up dissolved in the water, some will end up involved with the suspended sediment load but the rest will end up on the stream bottom where it will contribute P to water only over a long period of time. Complicating this is seasonal changes in capacity of a stream to carry suspended sediment. Clean water is hungry water and it picks up material fairly easily. Muddy water is different and it drops it's sediment load whenever it loses energy, the insides of curves for instance. You can bet that sediment delivered to a clean stream is going to affect total phosphorus levels more efficiently than sediment delivered to a muddy stream. Considerations of efficiency mean testing for available phosphorus may not be enough. The next most obvious analytes to add into the mix are total phosphorus, texture, pH and organic matter content. I'm looking forward to a lively discussion.


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