Saturday, November 16, 2013

Potassium nitrate: a versatile soluble fertilizer


Potassium nitrate (KNO3) is a soluble source of two major essential plant nutrients. It is commonly used as a fertilizer for high-value crops that benefit from nitrate (NO3-) nutrition and a source of potassium (K+) free of chloride (Cl-).
Prilled potassium nitrate

Production
Potassium nitrate fertilizer (sometimes referred to as nitrate of potash or NOP) is typically made by reacting potassium chloride (KCl) with a nitrate source. Depending on the objectives and available resources, the nitrate may come from sodium nitrate, nitric acid, or ammonium nitrate. The resulting KNO3 is identical regardless of the manufacturing process. Potassium nitrate is commonly sold as a water-soluble, crystalline material primarily intended for dissolving and application with water or in a prilled form for soil application. Traditionally, this compound is known as saltpeter.

Chemical Properties
Chemical formula:              KNO3
N content:                           13%
K2O content:                       44 to 46%
Water solubility (20°C):       316 g/L
Solution pH:                         7 to 10
 Agricultural Use
Potassium nitrate granules for dissolving
The use of KNO3 is especially desirable in conditions where a highly soluble, chloride-free nutrient source is needed. All of the N is immediately available for plant uptake as nitrate, requiring no additional microbial action and transformation in the soil. Growers of high value vegetable and orchard crops sometime prefer to use a nitrate-based source of nutrition in an effort to boost yield and quality. Potassium nitrate contains a relatively high proportion of K, with a N to K ratio of approximately 1:3. Many crops have high K demands and can remove as much or more K than N at harvest.

Applications of KNO3 to the soil are made before the growing season or as a supplement during the growing season. A diluted solution is sometimes sprayed on plant foliage to stimulate physiological processes or to overcome nutrient deficiencies. Foliar application of K during fruit development can be advantageous for some crops, since this growth stage often coincides with high K demands during the time of declining root activity and nutrient uptake. It is also commonly used for greenhouse plant production and hydroponic culture.

Management Practices
Both N and K are required by plants to support harvest quality, protein formation, disease resistance, and water use efficiency. Therefore, KNO3 is often applied to soil or through the irrigation system during the growing season to support healthy growth.
Potassium nitrate prills are white

Potassium nitrate accounts for only a small portion of the global K fertilizer market. It is primarily used where its unique composition and properties are able to provide specific benefits to growers. It is easy to handle and apply, and is compatible with many other fertilizers. This includes usage for many high-value specialty crops, as well as grain and fiber crops.
Water solubility of common potassium fertilizers

The relatively high solubility of KNO3 under warm conditions allows for a more concentrated solution than for other common K fertilizers. Careful water management is needed to keep the nitrate from moving below the root zone.

Non Agricultural Uses
Potassium nitrate has long been used for fireworks and gunpowder. It is now more commonly used in food to maintain the quality of meat and cheese. Specialty toothpastes often contain KNO3 to alleviate tooth sensitivity. A mixture of KNO3 and sodium nitrate (NaNO3) is used for storing heat in solar energy installations.

Monday, November 11, 2013

Potassium Magnesium Sulfate fertilizer: Langbeinite


Langbeinite is a unique source of plant nutrition since three essential nutrients are naturally combined into one mineral. It provides a readily available supply of K, Mg, and S to growing plants.


Production
Langbeinite is a distinctive geological material found in only a few locations in the world. Commercial supplies of lang­beinite come from underground mines near Carlsbad, New Mexico (USA), which were first commercially developed in the 1930s. These deposits were formed millions of years ago when a variety of salts, including langbeinite, were left behind after the evaporation of ancient ocean beds. These salt deposits were buried deep beneath hundreds of meters of sediment. The langbeinite deposit is currently mined with large boring machines, washed to remove impurities, and then crushed to various particle sizes. Langbeinite is considered a potash (or K-containing) fertilizer, even though it also contains valuable Mg and S. Traces of iron oxide impurities give some langbeinite particles a reddish tint.
Underground mining in New Mexico



 Chemical Properties
Property:                             K2SO4.2MgSO4
Fertilizer analysis:                  21 to 22% K2O
                                             10 to 11% Mg
                                             21 to 22% S
Water solubility (20 ºC)           240 g/L
Solution pH                            approx. 7

Agricultural Use
Langbeinite is a popular fertilizer, especially where several nutrients are needed to provide adequate plant nutrition. It has an advantage of having K, Mg, and S all contained within a single particle, which helps provide a uniform distribution of nutri­ents when it is spread in the field. Due to economics, langbeinite may not be recommended to meet the entire K requirement of a crop. Instead, application rate may be based on the need for Mg and/or S.

Langbeinite is totally water soluble, but is slower to dissolve than some other common K fertilizers because the particles are denser than other K sources. Therefore, it is not suitable for dissolving and application through irrigation systems unless finely ground. It has a neutral pH, and does not contribute to soil acidity or alkalinity. This differs from other common sources of Mg (such as dolomite) which will increase soil pH and from elemental S or ammonium sulfate which will lower the soil pH.

Langbeinite fertilizer
It is frequently used in situations where a fertilizer free of Cl- is desirable, such as with crops sensitive to Cl- (some vegeta­bles and certain tree crops). Langbeinite is a nutrient-dense fertilizer with a relatively low overall salt index. Particular sources of langbeinite have been certified for use in organic crop production in some countries.

Management Practices
Langbeinite has no restrictions for environmental or nutritional use when used at typical agronomic rates. One form of langbeinite is sold as a feed grade dietary source of K, Mg, and S for animals and poultry. All three of these nutrients are required for animal nutrition and each has a specific metabolic role required for optimal animal health. This feed material is “recognized as safe” by government agencies. As with all plant nutrients, best management practices should be observed to properly utilize this resource. A particular particle size should be matched with the specific need. 
Most potash fertilizers are extracted from great depths
Non-agricultural Use:
There are no major industrial applications for langbeinite outside of agriculture.

Some examples of commercial langbeinite fertilizers produced in North America include the products of K-Mag (Mosaic Co), and TRIO (Interpid Potash).

Monday, November 4, 2013

The Phosphorus Crisis: When Is It Coming, and Is There a Simple Solution?



 Don't believe everything you see and hear.





Biologist Mohamed Hijri presents an interesting TED talk entitled: 
A simple solution to the coming phosphorus crisis
 http://www.ted.com/talks/mohamed_hijri_a_simple_solution_to_the_coming_phosphorus_crisis.html

He talks about two issues associated with the phosphorus nutrition of plants. The first is the finite nature of phosphate reserves (the source of phosphorus fertilizer), and the second is algal blooms arising from losses of phosphorus from agricultural fields. We appreciate the recognition of the important role of phosphorus in supporting agricultural production for a future global population of over 9 billion.   But he presents many statements as fact without any supporting references. Many of these statements contradict a considerable volume of published peer-reviewed scientific and technical literature. IPNI welcomes discussion of issues associated with phosphorus fertilizer use, and the opportunity to clarify public perception of those issues. Applying the right source of phosphorus fertilizers at the right rate, right time and right place is consistent with maintenance of an appropriate level of mycorrhizae in agricultural soils. 

This statement of correction is posted in the IPNI website: http://www.ipni.net/article/IPNI-3344
 
Biologist Mohamed Hijri presents a very polished lecture in French on the important topic of two issues associated with the phosphorus nutrition of plants. The first is the finite nature of phosphate reserves; the source of phosphorus fertilizer, and the second is algal blooms arising from losses of phosphorus from agricultural fields.

While the lecture is well presented, certain statements are presented as fact without any reference to supporting literature. Here we point out that these statements contradict a considerable volume of published peer-reviewed scientific and technical literature

1. “There is a global phosphorus crisis, and no one is talking about it.” In recent years, there has been considerable international activity and discussion of phosphorus issues. One example is the organization called Global TraPs – the Global Transdisciplinary Processes for Sustainable Phosphorus Management, a multi-stake holder forum based jointly in Germany and the U.S. In addition, the International Fertilizer Development Center published a technical bulletin (Van Kauwenbergh, 2010) called “World Phosphate Rock Reserves and Resources” which, while highlighting the industry’s concern for finite resources, indicates that the figures used by Professor Hijri are out of date, and shows that current reserves are considerably larger, sufficient for over 300 years at current rates of extraction. The reserve figures in this publication are in agreement with the USGS (2013) publication of mineral commodity summaries. In addition, the International Plant Nutrition Institute has published a 2013 article “World Reserves of Phosphate Rock…a Dynamic and Unfolding Story” which points out that over the past decade or so there has been concern that the world would soon deplete its phosphate rock resources, and face a catastrophic phosphorus shortage; however, recent and thorough estimates of world supply indicate that a crisis is not imminent, and that we will not soon run out of phosphate rock.

2. “Peak phosphorus will occur by 2030 and all reserves will be gone by 2100.” As pointed out above, more recent published material (e.g. Scholz and Wellmer, 2013) and presentations show that this statement, usually attributed to Cordell (2009), is based on outdated reserve estimates and methodology and has been strongly criticized because it over estimates the urgency of the phosphorus supply risk. The modeling approach in the graph used to demonstrate the peak of phosphate production occurring in 2030 has also been shown to be inaccurate and unrealistic (Hendrix, 2011). In addition, Sutton et al. (2013; figure 2.9 on page 15) point out that many other important commodities, including crude oil and natural gas, and the important micronutrient zinc, have much shorter estimates for reserve life than does phosphate.

3. “Only 15% of [phosphorus fertilizer applied] goes to the plant. 85% is lost. It goes into the soil, ending its journey in the lakes.” While eminent soil fertility scientists recognize that soil reactions with applied phosphate limit its direct uptake by plants in the short term, the long term recovery can approach 90%, because phosphorus is retained in the soil in slowly available forms (Syers et al., 2008). Estimates of the global phosphorus cycle depicted in Figure 3.2 on page 23 of Sutton et al. (2013) indicate that the total transfer of phosphorus from the terrestrial ecosystem to fresh waters is considerably less than 85% of the total input of phosphorus to agricultural soils. It also indicates that much of this transfer arises from erosion, a process that carries indigenous soil phosphorus as well as that applied in the form of fertilizers. So, the actual loss of phosphorus from fertilizer is both smaller and less direct than indicated in the presentation by Professor Hijri. Industry is engaging 4R Nutrient Stewardship to reduce these losses; examples include a collection of articles under the topic of Lake Erie P Issues and a list of activities at www.nutrientstewardship.com.
4. The presentation suggests that a plant with mycorrhizae will take up 90% of applied phosphorus in comparison to the 15% taken up by plants in conventional agriculture. First, this comparison is misleading, since two factors are changing at once, both rate of application and mycorrhizal presence, and it is well known that recovery efficiencies decline as rates increase. An example of a study actually measuring change in phosphorus uptake caused by mycorrhizae is provided in Table 3 of Grant et al. (2005). Calculations from those data show that the mycorrhizal benefit to phosphorus recovery declining from 69% at low levels of P fertilization to no benefit at very high levels of P fertilization. This is a considerably smaller benefit than is implied by comparing the presented figures of 90% and 15% recovery, and does not take into account the yield losses associated with reduced levels of P fertilization. Second, the implication that plants grown in conventional crop production are without mycorrhizae is incorrect. Mycorrhizae are present in most soils when crops supporting them are grown. These crops include corn, soybeans, wheat and other cereals. Third, studies comparing plants with and without mycorrhizae in the field show much smaller increases in phosphorus uptake, often associated with lower yields. For example, research conducted near Montreal (Liu et al., 2003) showed that corn yield response to the presence of mycorrhizae was small (8%), occurring only when corn was not fertilized with phosphorus, while fertilization with phosphorus produced yield gains of up to 18%. In this experiment, fertilizing at recommended rates reduced mycorrhizal hyphae density by only 11%. Similar mutually beneficial effects of mycorrhizae and phosphorus fertilizer were shown in research conducted in British Columbia (Bittman et al., 2003). In certain low phosphorus soils of Australia, mycorrhizae have been shown to have parasitic activity, reducing the yields of crops (Ryan et al., 2005). The fertilizer industry’s 4R Nutrient Stewardship approach recognizes the value of mycorrhizae in crop production (IPNI, 2012 page 2-7). Applying the right source of phosphorus fertilizers at the right rate, right time and right place is consistent with maintenance of an appropriate level of mycorrhizae in agricultural soils.

We appreciate the recognition of the important role of phosphorus in supporting agricultural production for a future global population of over 9 billion. Industry welcomes discussion of issues associated with phosphorus fertilizer use. Improvements in the sustainability of such agricultural production depend on an accurate public perception of these issues, and thus we encourage Professor Hijri to correct the record on the four important points outlined above.

References
Bittman, S., C. G. Kowalenko, et al. 2006. Starter phosphorus and broadcast nutrients on corn with contrasting colonization by mycorrhizae. Agron J 98(2):394-401.

Cordell, Dana, Jan-Olof Drangert, and Stuart White. 2009. The story of phosphorus: Global food security and food for thought. Global Environmental Change 19:292–305.

Grant, C., Bittman, S., Montreal, M., Plenchette, C. and Morel, C. 2005. Soil and fertilizer phosphorus: Effects on plant P supply and mycorrhizal development. Can. J. Plant Sci. 85: 3–14.

Hendrix, C.S. 2011. Applying Hubbert curves and linearization to rock phosphate. Working Paper Series. WP 11-18. Peterson Institute for International Economics. Washington, DC. p. 12

IPNI. 2012. 4R Plant Nutrition Manual: A Manual for Improving the Management of Plant Nutrition, Metric Version, (T.W. Bruulsema, P.E. Fixen, G.D. Sulewski, eds.), International Plant Nutrition Institute, Norcross, GA, USA.

Liu, A., Hamel, C., Elmi, A. A., Zhang, T. and Smith, D. L. 2003. Reduction of the available phosphorus pool in field soils growing maize genotypes with extensive mycorrhizal development. Can. J. Plant Sci. 83: 737–744.

Ryan, M. H., A. F. van Herwaarden, et al. 2005. Reduced growth of autumn-sown wheat in a low-P soil is associated with high colonisation by arbuscular mycorrhizal fungi. Plant Soil 270(1-2): 275-286.

Scholz, R. and F.W. Wellmer. 2013. Approaching a dynamic view on the availability of mineral resources: what we may learn from the case of phosphorus? Global Environmental Change. 23:11-27

Sutton et al. 2013. Our Nutrient World: The challenge to produce more food and energy with less pollution.  Global Overview of Nutrient Management. Centre for Ecology and Hydrology, Edinburgh.

Syers, JK, AE Johnston, and D Curtin. 2008. Efficiency of soil and fertilizer phosphorus use. FAO Fertilizer and Plant Nutrition Bulletin 18. Food and Agriculture Organization of the United Nations, Rome, Italy.

USGS. 2013. Mineral commodity summaries. [Online]. Available at http://minerals.usgs.gov/minerals/pubs/
commodity/phosphate_rock/index.html#mcs (verified 19 April 2013).

Van Kauwenbergh, S.J. 2010. World Phosphate Rock Reserves and Resources. IFDC. Muscle Shoals, AL, USA. www.ifdc.org






Friday, November 1, 2013

The Facts about Phosphate Rock… Are We Running Out?


Most of the phosphate rock that is mined from the earth goes towards making fertilizer for
Phosphorus is a major component of bones and teeth
crop production.  Every cell in plants and animals requires phosphorus to sustain itself and there is no substitute for it in nature.

During the past five years, there were several well-publicized reports suggesting the world phosphate rock supply was rapidly dwindling.  In response, there was widespread concern about whether we were reaching our “peak” supply of phosphate rock and if fertilizer shortages are on the horizon.
Map of world phosphorus resources (IFDC)


Recently updated estimates report that the earth has at least 300 years of years of known phosphate rock reserves (recoverable with current technology) and 1400 years of phosphate rock resources (phosphate rock that may be produced at some time in the future).  These numbers fluctuate somewhat since companies do not intensively explore resources that will only be mined far in the future.


Phosphate fertilizer can be a significant cost for crop production and an important mineral for animals.  However from a global perspective, phosphate is considered as a low-price commodity.  One recent publication estimated that each person consumes an equivalent of 67 lb phosphate rock each year.  This results in an annual consumption of about 9 lb phosphorus per person (or 0.4 oz. daily consumption), which is equivalent to 1.7 cents per day.  



Generalized sedimentary  deposit


Phosphorus atoms do not disappear in a chemical sense, but they can be diluted in soil or water to the point where it is not economical to recover.  Annual phosphorus losses by erosion, manure, and human excrement to the sea roughly balance the phosphorus that is mined, showing that there is substantial room for improvement in efficiency.   Implementing appropriate recovery and recycling of phosphorus from animal manure, crop residue, food waste, and human excreta would make a major step in this direction. 

Efforts to improve phosphorus efficiency and building to the appropriate soil P concentrations  serves to enhance its use.  In developed countries with a history of adequate phosphorus fertilization, the need for high application rates diminishes over time.  This contrasts with the situation in many developing countries where low soil P concentrations still require significant fertilizer inputs to overcome crop deficiencies.
 

Rock phosphate mining in Florida

Members of the public are encouraged to engage in debate over important issues, but there is a danger that oversimplification leads to incorrect conclusions.  The case of looming P scarcity is an example where insufficient information lead to a wrong conclusion.  The wrong notion still persists that there is an impending shortage phosphorus and that limited fertilizer availability will soon lead to global food insecurity.

There may be a scarcity of many earth minerals some day, but the phosphorus supply will not be a concern for hundreds of years.   However responsible stewardship of rock phosphate resources requires a close examination of improving efficiency throughout the entire process, including mining, fertilizing crops, and implementing strategic waste recovery.
Rock phosphate mining in North Carolina


Thursday, October 31, 2013

Single Superphosphate - SSP, the first commercial mineral fertilizer



Single superphosphate (SSP) was the first commercial mineral fertilizer and it led to the development of the modern plant nutrient industry. This material was once the most commonly used fertilizer, but other phosphorus (P) fertilizers have largely replaced SSP because of its relatively low P content.
Typical single superphosphate

Production

The modern fertilizer industry was launched in the 1840s with discovery that the addition of sulfuric acid to naturally oc­curring phosphate produced an excellent soluble fertilizer, given the name superphosphate. Ground animal bones were first used in this reaction, but natural deposits of rock phosphate (apatite) soon replaced the limited supply of bones. Making SSP is similar to what naturally occurs with bones or apatite in acid soils. The basic technique has changed very little in the past century. Ground phosphate rock is reacted with sulfuric acid to form a semi-solid which cools for several hours in a den. The plastic-like material is then conveyed to a storage pile for several weeks of additional curing. The hardened material is then milled and screened to the appropriate particle size or granulated.

The general chemical reaction is:
Ca3(PO4)2 [rock phosphate] + 2 H2SO4 [sulfuric acid] → 

Ca(H2PO4)2 [monocalcium phosphate] + 2 CaSO4 [gypsum

Close up of single superphosphate
 SSP can easily be produced on a small scale to meet regional needs. Since SSP contains both monocalcium phosphate (MCP, also called calcium dihydrogen phosphate) and gypsum, there are no issues with phosphogypsum by-product dis­posal as occurs with the manufacture of other common P fertilizers. 

SSP is also known as ordinary superphosphate and normal superphosphate. It is sometimes confused with triple super­phosphate (TSP) production, which is made by reacting rock phosphate with phosphoric acid.

Chemical Properties
Phosphorus content:             7 to 9% (16 to 20% P2O5)
Calcium (Ca) content:           18 to 21%
S content:                             11 to 12%
pH:                                         < 2

Agricultural Use 
SSP is an excellent source of three plant nutrients. The P component reacts in soil similarly to other soluble fertilizers. The presence of both P and sulfur (S) in SSP can be an agronomic advantage where both of these nutrients are deficient. In agronomic studies where SSP is demonstrated to be superior to other P fertilizers, it is usually due to the S and/or Ca that it contains. When locally available, SSP has found wide-spread use for fertilizing pastures where both P and S are needed. As a source of P alone, SSP often costs more than other more concentrated fertilizers, therefore it has declined in popularity. 
 
Single superphosphate granules
Management Practices
No special agronomic or handling precautions are required for SSP. Its agronomic effectiveness is similar to other dry or liquid phosphate fertilizers.
The loss of P in surface runoff from fertilized fields can contribute to water quality problems. Farm practices that minimize this loss should be implemented. 

Non Agricultural Uses
SSP is primarily used as a crop nutrient source. However MCP and gypsum (the two primary ingredients in SSP) are widely used in many products. For example MCP is commonly added to enrich animal feed. It is also routinely used as a leavening agent to cause baked goods to rise. Gypsum is widely used in the construction industry, as well as in the food and pharmaceuticals.
 

Sunday, August 18, 2013

What Is Sustainable Anyway?


The pathway to "sustainability" is not always clear
Sustainability is a phrase that gets thrown around so frequently that there is little consideration about what the word really means. After all, who can be opposed to sustainable agriculture?

Sustainability was famously described as meeting the needs of the present without compromising the ability of future generations to meet their own needs.

The vision of sustainable agriculture is more philosophical than a well-defined goal. It certainly includes the stewardship of natural resources, financial security for farmers, and consideration of societal goals. However since there is no agreement on how to achieve these objectives, these terms can be twisted to meet personal agendas.
Using all nutrients efficiently should be a top goal


Many will agree that each person has an individual preference on how to balance current consumption with future enjoyment. Frequently we want things now, instead of waiting for a future reward. Some people are careful savers for the future, while others spend all that they earn. Achieving sustainability is a flexible goal that reflects individual priorities and incentives. There are also regional considerations that must be factored into sustainability objectives.
Providing an adequate food supply


The unprecedented pressure on the global food supply to meet the growing population requires close examination of all our current practices. Our soil and water resources are under severe stress in some areas. Like all geologic resources, the supply of phosphate and potash is fi nite in the world. Although there is no risk of fertilizer shortage in the next centuries, consideration of appropriate conservation and recycling practices should always be in the forefront of their use. Modern food systems require the input of considerable energy. There are numerous changes that can be made to make our food supply more sustainable.
Phosphate mining provides needed nutrients


Some groups promote a return to organic fertilization practices, other voices suggest that agroecology or integrated nutrient management is the path towards sustainability. Being dogmatic about a single solution causes more conflict than progress. There is no single path towards achieving agricultural sustainability.

Human nutrition is part of sustainability
IPNI is dedicated to the development and delivery of the best scientific information about the responsible use of plant nutrients. Instead of arguing over which definition of agricultural sustainability is correct, let’s get on with the task of using plant nutrients as efficiently and effectively as possible.
Growing adequate fiber and fuel also needs attention

 This article first appeared in the IPNI magazine, Better Crops (available here)