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Minerals and Crushed Rock - A TerraSoil Overview

TerraSoil

03 Aug 2024

Harnessing the Power of Naturally Mined Minerals, Clays, and Crushed Rocks in Agriculture

Rocks in Agriculture?

The use of naturally mined minerals, clays, and crushed rocks in agriculture, often termed as rock dust application, has garnered significant attention for its potential to enhance soil fertility, improve plant health, and contribute to sustainable farming practices. This overview highlights the benefits of rock dust application in agriculture, the types of minerals used, their chemical compositions, and their specific benefits to plants, soil structure, and soil microfauna. Additionally, it highlights how microbes and fungi facilitate nutrient availability from rock dust and discusses the sustainability benefits of using these natural amendments.


Benefits of Rock Dust Application in Agriculture

Rock dust application in agriculture provides multiple benefits:

  1. Nutrient Enrichment: Rock dust releases a broad spectrum of essential minerals and trace elements into the soil, improving nutrient availability for plants.

  2. Soil Structure Improvement: It enhances soil texture, aeration, and water retention and promotes healthier root systems.

  3. Microbial Activity Enhancement: Rock dust fosters a thriving soil microbial community, crucial for nutrient cycling and soil health.

  4. Disease Resistance: Improved soil health and nutrient availability can enhance plant resistance to pests and diseases​.

 

Rock and Mineral Types Used in Agriculture

The following table outlines common rock and mineral types used in agriculture, their chemical structures, and specific benefits:

Rock/Mineral Type

Chemical Structure

Specific Benefits

Basalt

Primarily composed of SiO₂ (silicon dioxide), Fe₂O₃ (iron(III) oxide), MgO (magnesium oxide), CaO (calcium oxide), Al₂O₃ (aluminum oxide), TiO₂ (titanium dioxide), MnO (manganese(II) oxide), Na₂O (sodium oxide), K₂O (potassium oxide)

Provides slow-release nutrients, improves soil structure by adding mineral content, enhances microbial activity, supplies essential macronutrients like calcium and magnesium, and trace minerals like manganese and iron which are vital for plant health.

Limestone

CaCO₃ (calcium carbonate)

Raises soil pH by neutralizing acidity, provides calcium which is crucial for cell wall strength in plants, improves soil structure by creating better aeration and drainage conditions, and reduces soil toxicity by buffering acidic conditions.

Granite Dust

Composed mainly of SiO₂ (silicon dioxide), K₂O (potassium oxide), Na₂O (sodium oxide), Al₂O₃ (aluminum oxide), Fe₂O₃ (iron(III) oxide), CaO (calcium oxide), MgO (magnesium oxide), TiO₂ (titanium dioxide), P₂O₅ (phosphorus pentoxide)

Supplies potassium and trace elements necessary for plant growth, improves soil texture by enhancing aeration and drainage, and enhances nutrient availability through slow mineral dissolution, providing a steady supply of essential nutrients.

Zeolite

Hydrated aluminosilicates of alkali and alkaline earth metals with a typical formula of (Na₂,K₂,Ca)₃Al₂Si₃O₁₀•2H₂O

Enhances cation exchange capacity (CEC), allowing soils to hold more nutrients, improves nutrient and water retention by trapping them in its porous structure, detoxifies soil by capturing heavy metals and toxins, and provides a beneficial environment for root growth.

Gypsum

CaSO₄•2H₂O (calcium sulfate dihydrate)

Provides calcium and sulfur, essential nutrients for plant development, improves soil structure by breaking up compacted soil layers and promoting root penetration, alleviates soil compaction and crusting, and aids in leaching excess sodium from the soil to improve its physical properties.

Glacial Rock Dust

Contains a wide range of minerals including SiO₂ (silicon dioxide), Fe₂O₃ (iron(III) oxide), MgO (magnesium oxide), CaO (calcium oxide), K₂O (potassium oxide), Na₂O (sodium oxide), and trace elements

Provides a diverse array of trace elements that support plant health and productivity, enhances microbial activity by supplying nutrients and improving soil health, boosts overall soil fertility, and improves plant growth by offering a broad spectrum of nutrients.

Diatomaceous Earth

Primarily composed of SiO₂ (silicon dioxide), with smaller amounts of Al₂O₃ (aluminum oxide), Fe₂O₃ (iron(III) oxide), Na₂O (sodium oxide)

Enhances soil aeration and drainage due to its porous structure, improves water retention while preventing waterlogging, controls pests by physically damaging their exoskeletons, and provides silica which strengthens plant tissues and enhances resistance to disease.

Phosphate Rock

Consists mainly of Ca₃(PO₄)₂ (calcium phosphate), CaO (calcium oxide), SiO₂ (silicon dioxide), Al₂O₃ (aluminum oxide), Fe₂O₃ (iron(III) oxide)

Supplies phosphorus, essential for energy transfer, photosynthesis, and root development, provides trace minerals necessary for plant health, and contributes to overall soil fertility and productivity.

Clay Minerals

Varies, but often includes kaolinite (Al₂Si₂O₅(OH)₄), illite (K,H₃O)(Al,Mg,Fe)₂(Si,Al)₄O₁₀(OH)₂•nH₂O, and montmorillonite ((Na,Ca)₀.₃(Al,Mg)₂Si₄O₁₀(OH)₂•nH₂O)

Improves soil texture by increasing water retention and nutrient holding capacity, supports beneficial microbial life by providing a stable environment, and enhances nutrient availability by adsorbing and releasing them slowly to plants.

Silicate Minerals

Includes various compositions such as olivine ((Mg,Fe)₂SiO₄), feldspars (e.g., orthoclase KAlSi₃O₈), and micas (e.g., muscovite KAl₂(AlSi₃O₁₀)(OH)₂)

Improves plant resistance to pests and diseases by strengthening cell walls, enhances soil structure by contributing to mineral diversity, releases essential nutrients like potassium, magnesium, and iron slowly, and helps to buffer soil pH levels.

Benefits of Applying Rock Dust to Plants, Soil Structure, and Soil Microfauna

  1. Plants: Rock dust provides essential macro and micronutrients, promoting vigorous plant growth and higher yields. The slow-release nature of these nutrients ensures a steady supply, reducing the risk of nutrient deficiencies or nutrient toxicity.

  2. Soil Structure: By improving soil texture, rock dust enhances soil aeration and water retention. Through the use of different particle sizes, the soil characteristics can be shifted towards a loam. The UN has a soil texture chart that allows users to identify their current soil type and how o shift the characteristics in a favourable direction. Correct soil texture for the plant species promotes healthy root development and reduces soil erosion​.

  3. Soil Microfauna: Rock dust fosters a beneficial environment for soil microorganisms, which are crucial for nutrient cycling and organic matter decomposition. Microbes are able to release nutrients through the use of organic acids and Cell surface redox reaction through Extracellular Electron transfer. Microbes have the ability to oxidise and reduce metal ions thereby affecting the solubility and plant availability of the nutrients. The paper xxxx also showed that electroactive microbes extracted from the roots of sweet potato were shown to improve the efficiency of redox reactions in laboratory setting by 100x.The research suggest that microbial biofilm production and protein nano-wires increases the effective area for electron transfer. Ultimately, enhanced microbial activity leads to healthier, more fertile soils.


How Microbes and Fungi Facilitate Nutrient Availability

Soil microbes and fungi play a pivotal role in making nutrients from rock dust available to plants:

  1. Mineral Weathering: Microorganisms secrete organic acids and enzymes that break down minerals in rock dust, releasing nutrients into the soil.

  2. Redox Reactions: Microorganisms use extracellular electron transfer to influence the solubility and plant availability of different elements.

  3. Symbiotic Relationships: Mycorrhizal fungi form symbiotic associations with plant roots, increasing the surface area for nutrient absorption and facilitating the uptake of minerals from rock dust. As specialist decomposers, fungi are able to breakdown complex compounds into usable forms, something plants cannot do on their own.

  4. Nutrient Cycling: Microbes and fungi decompose organic matter, releasing nutrients in forms that plants can readily absorb​. In the case of fungi, there is the mutualistic exchange of sugars for nutrients and water.

 

Sustainability Benefits of Using Rock Dusts in Agriculture

  1. Reduced Chemical Fertilizer Use: By providing a natural source of nutrients, rock dust reduces the dependence on synthetic fertilizers, which are energy-intensive to produce and can harm the environment through run-off or nutrient imbalance.

  2. Enhanced Soil Health: Regular application of rock dust improves soil structure and fertility, promoting long-term agricultural productivity. Once soil is in ideal conditions, the best application of rock dust would be in larger particle sizes so that the soil doesn’t shift towards a more clay texture.

  3. Carbon Sequestration: Certain rock types, like basalt, can capture and store atmospheric CO2 through a process known as enhanced weathering, contributing to climate change mitigation​.


 

Conclusion

The application of naturally mined minerals, clays, and crushed rocks in agriculture offers numerous benefits, from enhancing plant growth and soil health to promoting sustainable farming practices. By understanding the specific advantages of various rock types and the mechanisms through which they improve soil fertility, farmers can make informed decisions that support both agricultural productivity and environmental stewardship.


References

  1. Blum, J. D., & Erel, Y. (2005). "Rivers as Indicators of Chemical Weathering." Reviews in Mineralogy and Geochemistry, 59(1), 533-556.

  2. Jacks, G., & Sharma, V. P. (1983). "Geochemistry of Base Cations in Rainwater." Water Resources Research, 19(5), 1313-1320.

  3. Hinsinger, P. (2001). "Bioavailability of soil inorganic P in the rhizosphere as affected by root-induced chemical changes: A review." Plant and Soil, 237, 173-195.

  4. Basak, B. B., & Biswas, D. R. (2010). "Influence of Potassium Solubilizing Microorganisms (KSM) on Potassium Uptake Dynamics by Chrysanthemum (Chrysanthemum indicum L.) in Inceptisols of West Bengal." Indian Journal of Agricultural Sciences, 80(1), 2-7.

  5. Mäder, P., & Berner, A. (2012). "Development of reduced tillage systems in organic farming in Europe." Renewable Agriculture and Food Systems, 27(1), 7-15.

  6. Shepherd, T. G., Saggar, S., Newman, R. H., Ross, C. W., & Dando, J. L. (2001). "Tillage-induced changes to soil structure and organic carbon fractions in New Zealand soils." Australian Journal of Soil Research, 39(3), 465-489.

  7. Boul, S. W., Southard, R. J., Graham, R. C., & McDaniel, P. A. (2011). Soil Genesis and Classification. John Wiley & Sons.

  8. Hinsinger, P., & Courchesne, F. (2008). "Biogeochemistry of metals in the rhizosphere." Springer-Verlag, 123-128.

  9. Manning, D. A. C. (2010). "Mineral sources of potassium for plant nutrition. A review." Agronomy for Sustainable Development, 30(2), 281-294.

  10. Scherr, S. J., & Sthapit, S. (2009). "Mitigating Climate Change Through Food and Land Use." Worldwatch Report 179, Worldwatch Institute.

  11. White, R. E., & Rengel, Z. (2008). "Role of phosphorus in root growth and development." Plant and Soil, 312, 1-17.

  12. Lal, R. (2004). "Soil Carbon Sequestration Impacts on Global Climate Change and Food Security." Science, 304(5677), 1623-1627.

  13. Hinsinger, P., & Jaillard, B. (1993). "Root-induced release of interlayer potassium and vermiculitization of phlogopite as related to potassium depletion in the rhizosphere of ryegrass." Journal of Soil Science, 44, 19-27.

  14. Weismann, D., & Wesemael, B. (2009). "Soil and Climate Change: Modifying Our Approach to Soil Management." Environmental Science & Policy, 12(6), 569-577.

  15. Hallmann, J., & Berg, G. (2006). "Microbial Stress Management in the Rhizosphere." Soil Biology and Biochemistry, 38, 2153-2162.

  16. Johnson, N. C., Wilson, G. W. T., Bowker, M. A., Wilson, J. A., & Miller, R. M. (2010). "Resource limitation is a driver of local adaptation in mycorrhizal symbioses." Proceedings of the National Academy of Sciences, 107(5), 2093-2098.

  17. Eric M Conners., Karthikeyen Rengasamy., & Arpita Bose (2022). “Electroactive biofilms: how microbial electron transfer enables bioelectrochemical applications.” Journal of Industrial Microbiology and Biotechnology, 49(4)


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