Research and Practical Insights into Using Gypsum
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1 v e o m r p e n m I t l S i y o m S t p s o e sium: w d i M Research and Practical Insights into Using Gypsum Gypsum Effects on Soils Dr. Harry Schomberg Ecologist Phil Campbell Sr. Natural Resource Conservation Center, USDA-Agricultural Research Service BRAND GYPSUM
2 Gypsum Effects On Soils Harry Schomberg Watkinsville USDA, Agricultural Research Service J. Phil Campbell, Sr. Natural Resource Center Watkinsville, GA 2
3 Brief Outline Sources Soils background Role of gypsum in soils Plant nutrients Subsoil acidity Soil Sodic soils 3
4 Sources of Gypsum Geologic deposits By- product of electricity By- product of phosphorus mining Recycled gypsum Recycled drywall gypsum 4
5 Flue Gas Gypsum By- product from scrubbing of SO 2 gases from coal- fired power plants Wide- range of poten@al agricultural applica@ons 5
6 and Demand U.S. Gypsum Produc8on (mil tons) Mined Synthe8c Import Manufacturing markets cannot absorb all FGD gypsum at peak production 50 U.S. Gypsum Consump8on (mil tons) Source USGS
7 Gypsum Benefits in Agriculture Source of Ca and S for plant nutri@on Ameliorate subsoil acidity and Al 3+ toxicity Reduce P loss in runoff Flocculate clays to improve soil structure Reclaim sodic soils Decrease ph of sodic soils 7
8 Soil Physical Improves crust and seal organic ma_er stability soil and water erosion water and water use efficiency loss of nutrients, sediment and agricultural chemicals Stable aggregates runoff Unstable aggregates 8
9 Soil Chemical Alleviate subsoil acidity Improves water and nutrient use Improves crop yield and quality Remediate saline and sodic soils Improves crop Important in some areas of South Sodic affected field near Teoc, MS 9
10 of Gypsum Solubility Gypsum 2.5 g/l Ag Lime 1.73 g/l NaCL 14.9 g/l Ca ++ clay SO complex ion forma@on 10
11 Plant Ca and S Plants require rela@vely large amounts of Ca and S Ca 0.5% shoot dry weight S 0.1% to 0.5% dry weight for op@mal growth No Gypsum Gypsum 11
12 SOIL The Fundamental Concepts 12
13 Soil Components Mineral Organic ma_er Water Air Organisms 13
14 Soil Components 4 parts of soil About ½ of the soil volume is solid par@cles Mineral Matter 45% Soil Air 25% Soil Water 25% About ½ of the soil volume is pore space 14 Organic Matter 5%
15 Mineral Components 1/100 in Sand in mm Silt in mm Clay Less than in Less than mm Determine textural property of the soil Coarse textured, loose (more sand, less clay) Fine textured, heavy (more clay, less sand) Loamy (more even mix of sand, silt and clay 15
16 Soil Texture An8go Silt Loam 16
17 Soil Structure The arrangement of sand, silt, and clay particles to form larger aggregates. Organic matter is the glue that holds the aggregates together Large pores (spaces) between aggregates are filled with air in a moist soil. 1/10 inch Small pores are filled with water in a moist soil. Even smaller pores inside the aggregates (not shown) are also filled with water. 17
18 Soil Structure Examples of Soil Structure Granular (Subangular) Blocky (Angular) Platy Prismatic Columnar Wedge 18
19 on Soil Clays Calcium, +2 Magnesium, +2 Potassium, +1 Ammonium, +1 Sodium, +1 Copper, +2 Aluminum, +3 Hydrogen, +1 19
20 Exchange Capacity (CEC) is the total amount of cations a soil can retain Higher CEC greater ability to store plant nutrients Soil CEC increases With clay content With organic ma_er content With soil ph (to a point) 20
21 Soil 21
22 Agriculture in the Southern USA 25 million acres crop and pasture land Soils highly weathered Low nutrient and water holding capacity Impaired water bodies by contaminants (sediment, nutrients, agricultural chemicals) Green dots represent 25,000 acres of cropland. Source NRCS 22
23 Southern USA Soils Sands to clay loams Low of basic (Ca, Mg, K) Very acid subsoils with toxic levels of Al 3+ Cecil Soil NRCS Photo Tikon Soil NRCS Photo 23
24 of Southern Soils Weak structure Crust prone Low & high runoff rates Low nutrient & water Highly Erodible 24
25 Soil Acidity Top- and subsoil acidity Excess Al and Mn Deficient Ca Root extension and Require adequate Ca Limited by toxic levels of Al Poor root system Limited water and nutrient uptake Low yields 25
26 phcacl 2 vs. KCl Extractable Al KCl Extr. Al (mg/kg) Cri8cal ph 4.85 For Saturated Paste NAPT Soils Soil ph (1:1) CaCl 2 Miller et al
27 Depth inches Soil ph w vs depth Crisp County Site 1 Site 2 Site 3 Site 4 Site 5 Site Kissel,
28 Ca and Root Growth in Acid Subsoils Phloem immobile Is not translocated to lower root even if topsoil is adequately limed Ca from gypsum leaches to subsoil reduces toxic Al 3+ Allows be_er root Allows be_er of subsoil water Translates into increased yields 28
29 of Subsoil Acidity and Al 3+ Toxicity Surface- applied gypsum leaches down to subsoil Ca 2+ exchanges with Al 3+ SO 4 2- forms complex ion AlSO 4 + with Al 3+ AlSO 4 + is not toxic to plant roots 29
30 of Subsoil Acidity Crop Gypsum Applica8on Al 3+ Al 3+ Al 3+ Al 3+ Al 3+ Al 3+ Ca 2+ Ca 2+ Ca 2+ Ca 2+ Ca 2+ Ca 2+ Ca 2+ Ca 2+ Ca 2+ Ca 2+ Ca 2+ Ca 2+ Al 3+ Al 3+ Al 3+ Al 3+ Al3 + Al 3+ Al 3+ Al 3+ Al 3+ 30
31 Soil Profile Ca and S Aker 3 Years Ca (g/kg) S (g/kg) Depth (inches) t/a 1 t/a 2 t/a 3 t/a Depth (inches) t/a 1 t/a 2 t/a 3 t/a t/a 1 t/a 2 t/a 3 t/a 25 Rhoton
32 Soil Profile Al and ph Aker 3 Years 0 Al (g/kg) ph Depth (inches) t/a 1 t/a 2 t/a 3 t/a Depth (inches) t/a 1 t/a 2 t/a 3 t/a Rhoton
33 Co_on Root Development - Mississippi Contorted tap roots due to Al toxicity Straight tap roots in absence of Al 33
34 Effect of Gypsum on Co_on Yield & Value Treatment 2000 Lint CoYon Yield (lb/acre) Control Gypsum Difference Value Profit $ $218 $ , $224 $ $50.00 $ $ $ Sumner 34
35 Bermudagrass Root Growth Root Weight (lb/ac) to 6 in 5 Control 6 to 12 in Depth (inches) Gypsum 12 to 18 in Bermudagrass Sumner & Larrimore 35
36 Poultry in the US 7.8 Billion Broilers 33 Million Tons Poultry Li_er 36
37 Poultry In the South GA, AR, AL, MS & NC 4.9 billion broilers 21 million tons broiler li_er 289,000 tons N 277,000 tons P 37
38 Excess Manure P NRCS
39 FGD Gypsum to Remediate High Soil P Nitrogen Phosphorus 39
40 FDG Gypsum and Phosphorus Concentra8on (mg/l) Broiler LiYer Treated Soil Total P PO4 Control Gypsum Franklin et al.,
41 Impact of FGD- Gypsum Mississippi River tons P day - 1 Reduce P loss from PL by 4,000 tons yr - 1 in Southern States 41
42 Gypsum and Clay Reduces soil Improves water Improves water transmission 42
43 and Dispersion Flocculated clay Dispersed clay Ca 2+ HOH Na+ Clay particle 43
44 Soil aggregates - - cemented clusters of sand, silt, and clay Flocculated Par@cles Dispersed Par@cles 44
45 allows water and plant roots to penetrate the soil 45
46 Dispersed clays plug soil pores and impede water and soil drainage. 46
47 Poorly Structured Soil Gypsum CaSO Na + Ca 2+ SO SAR EC Increasing soluble calcium improves aggregate stability Flocculated soil Dispersed soil 47
48 Gypsum & Rainfall Miller & Scirefs
49 FGD Gypsum Influence on Soil ton/acre ton/acre Floccula@on of the Bonn soil at the end of first cropping season Rhoton, ton/acre ton/acre 49
50 Gypsum in of Sodic Soils Sodic soil are dominated by excessive exchangeable Na Ca to replace exchangeable Na Salt to maintain electrolyte at soil surface Prevents (reduces) clay dispersion and swelling Maintains good surface rate 50
51 Ion Relative Flocculating Power Sodium Na Potassium K Magnesium Mg Calcium Ca We can divide ca@ons into two categories Poor flocculators Sodium Good flocculators Calcium Magnesium Sumner and Naidu,
52 Soil Classification EC SAR Condition Normal <4 <13 Flocculated Saline >4 <13 Flocculated Sodic <4 >13 Dispersed Saline-Sodic >4 >13 Flocculated 52
53 Flocculated Soil Soil will flocculate if of (Ca 2+ + Mg 2+ ) are increased rela@ve to the concentra@on of Na + (SAR is decreased) Na + Ca 2+ and Mg SAR EC Flocculated soil Dispersed soil 53
54 Dispersed Soil Ca 2+ and Mg 2+ Soil will disperse if of (Ca 2+ + Mg 2+ ) are decreased rela@ve to the concentra@on of Na + (SAR is increased). SAR Na + EC Flocculated soil Dispersed soil 54
55 Gypsum on Sodium Affected Soils Apply before leaching salts out of soils to dispersion v Amount needed can be determined by a soil test v Replacing sodium before leaching stabilizes soil structure. Ca 2+ SO 4 2- Ca ++ Ca Ca ++ Ca ++ Na + Na + Na + Na Na - + Na Na Na + Na + + Na + Na + Na Na + + Na + Na + Na + 55
56 Acknowledgments Dr. Malcolm Sumner University of Georgia Mr. Lamar Larrimore Southern Company Dr. James Walworth University of Arizona Dr. Bill Miller University of Georgia Dr. Fred Rhoton ARS Oxford, MS Dr. Dory Franklin ARS Watkinsville, GA Dr. David Kissel University of Georgia NRCS Soils Team & Support Staff of the ARS J. Phil Campbell, Natural Resource Center, Watkinsville GA 56
57 57
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