306-9 Changes in pH and Mehlich-3 Extractable Nutrients of Selected Soils From the Midwest and South USA As Influenced by Different Rates of Iron Calcium Silicate Slag.

Poster Number 2226

See more from this Division: S08 Nutrient Management & Soil & Plant Analysis
See more from this Session: Lime, Gypsum, and by-Product Utilization
Tuesday, October 23, 2012
Duke Energy Convention Center, Exhibit Hall AB, Level 1
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Brenda Tubana, School of Plant, Environmental, and Soil Sciences, Louisiana State University AgCenter, Baton Rouge, LA, Narayanaswamy Chowdappa, Indian Farmers Fertilizer Cooperative in Karnataka India / Louisiana State University AgCenter, Baton Rouge, LA, Lawrence Datnoff, Department of Plant Pathology and Crop Physiology, Louisiana State University AgCenter, Baton Rouge, LA and John Yzenas, Solutions Group, Edward Levy Corporation, Dearborn, MI
Calcium silicate (CaSiO3) slag is among the sources of silicon (Si) in crop production and commonly obtained as by-products in steel industry and production of elemental P. These slag by-products have high calcium carbonate equivalent (CCE) making them also suitable as liming material. In the USA, CaSiO3 slag is commonly apply to soil cultivated for rice and sugarcane production at quantities ranging between 1 MT to as high as 6 MT ha-1. With high application rates and high CCE value of CaSiO3 slag, the solubility of essential nutrients such as P, Zn, Fe and Mn can be altered. This study was conducted to quantify the effect of different rates of iron and steel CaSiO3 slag by-product (17% Si, 81% CCE) on soil pH and extractable elements of soils collected from the Midwest and South USA. Soils were acidic (pH 5.0) to slightly alkaline (pH 7.4) with wide ranges of Mehlich-3 (M3) extractable macro- and micro-nutrients. Bulk soil samples were processed and placed in 2-kg capacity pots where CaSiO3 slag rates of 0, 1, 2, 4, 6 and 8 MT ha-1 were thoroughly mixed with the top 15-cm surface of the potted soil. Soil samples were collected after allowing ryegrass to grow for 3 months. The pH of several soils increased linearly with increasing rates of CaSiO3; these soils either had initially low pH or classified as coarse-textured soils. The highest change in pH before and after CaSiO3 application was a unit of 1.05 for soils which received 8 MT CaSiO3 ha-1. Mehlich-3 extractable Mg, Mn, S, and Ca of all the soils increased with increasing rates of CaSiO3 slag. This can be attributed to the large concentrations of these elements contain in the slag material. The steady decline of M3-extractable Fe and Ni (and Zn in some soils) may be related to the potential of CaSiO3 slag to raise soil pH, hence decreasing the solubility of these metal cations. Our results show that both liming potential and composition of CaSiO3 slag had significant effect on the amount of M3-extractable essential nutrients.
See more from this Division: S08 Nutrient Management & Soil & Plant Analysis
See more from this Session: Lime, Gypsum, and by-Product Utilization
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