Soil acidification and the importance of liming agricultural soils with particular reference to the United Kingdom
Soil acidification is caused by a number of factors including acidic precipitation and the deposition from the atmosphere of acidifying gases or particles, such as sulphur dioxide, ammonia and nitric acid. The most important causes of soil acidification on agricultural land, however, are the applica...
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| Published in | Soil use and management Vol. 32; no. 3; pp. 390 - 399 |
|---|---|
| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
England
Blackwell Publishing Ltd
01.09.2016
Wiley Subscription Services, Inc John Wiley and Sons Inc |
| Subjects | |
| Online Access | Get full text |
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| Abstract | Soil acidification is caused by a number of factors including acidic precipitation and the deposition from the atmosphere of acidifying gases or particles, such as sulphur dioxide, ammonia and nitric acid. The most important causes of soil acidification on agricultural land, however, are the application of ammonium‐based fertilizers and urea, elemental S fertilizer and the growth of legumes. Acidification causes the loss of base cations, an increase in aluminium saturation and a decline in crop yields; severe acidification can cause nonreversible clay mineral dissolution and a reduction in cation exchange capacity, accompanied by structural deterioration. Soil acidity is ameliorated by applying lime or other acid‐neutralizing materials. ‘Liming’ also reduces N2O emissions, but this is more than offset by CO2 emissions from the lime as it neutralizes acidity. Because crop plants vary in their tolerance to acidity and plant nutrients have different optimal pH ranges, target soil pH values in the UK are set at 6.5 (5.8 in peaty soils) for cropped land and 6.0 (5.3 in peaty soils) for grassland. Agricultural lime products can be sold as ‘EC Fertiliser Liming Materials’ but, although vital for soil quality and agricultural production, liming tends to be strongly influenced by the economics of farming. Consequently, much less lime is being applied in the UK than required, and many arable and grassland soils are below optimum pH. |
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| AbstractList | Soil acidification is caused by a number of factors including acidic precipitation and the deposition from the atmosphere of acidifying gases or particles, such as sulphur dioxide, ammonia and nitric acid. The most important causes of soil acidification on agricultural land, however, are the application of ammonium-based fertilizers and urea, elemental S fertilizer and the growth of legumes. Acidification causes the loss of base cations, an increase in aluminium saturation and a decline in crop yields; severe acidification can cause nonreversible clay mineral dissolution and a reduction in cation exchange capacity, accompanied by structural deterioration. Soil acidity is ameliorated by applying lime or other acid-neutralizing materials. 'Liming' also reduces N sub(2)O emissions, but this is more than offset by CO sub(2) emissions from the lime as it neutralizes acidity. Because crop plants vary in their tolerance to acidity and plant nutrients have different optimal pH ranges, target soil pH values in the UK are set at 6.5 (5.8 in peaty soils) for cropped land and 6.0 (5.3 in peaty soils) for grassland. Agricultural lime products can be sold as 'EC Fertiliser Liming Materials' but, although vital for soil quality and agricultural production, liming tends to be strongly influenced by the economics of farming. Consequently, much less lime is being applied in the UK than required, and many arable and grassland soils are below optimum pH. Soil acidification is caused by a number of factors including acidic precipitation and the deposition from the atmosphere of acidifying gases or particles, such as sulphur dioxide, ammonia and nitric acid. The most important causes of soil acidification on agricultural land, however, are the application of ammonium‐based fertilizers and urea, elemental S fertilizer and the growth of legumes. Acidification causes the loss of base cations, an increase in aluminium saturation and a decline in crop yields; severe acidification can cause nonreversible clay mineral dissolution and a reduction in cation exchange capacity, accompanied by structural deterioration. Soil acidity is ameliorated by applying lime or other acid‐neutralizing materials. ‘Liming’ also reduces N 2 O emissions, but this is more than offset by CO 2 emissions from the lime as it neutralizes acidity. Because crop plants vary in their tolerance to acidity and plant nutrients have different optimal pH ranges, target soil pH values in the UK are set at 6.5 (5.8 in peaty soils) for cropped land and 6.0 (5.3 in peaty soils) for grassland. Agricultural lime products can be sold as ‘ EC Fertiliser Liming Materials’ but, although vital for soil quality and agricultural production, liming tends to be strongly influenced by the economics of farming. Consequently, much less lime is being applied in the UK than required, and many arable and grassland soils are below optimum pH . Soil acidification is caused by a number of factors including acidic precipitation and the deposition from the atmosphere of acidifying gases or particles, such as sulphur dioxide, ammonia and nitric acid. The most important causes of soil acidification on agricultural land, however, are the application of ammonium-based fertilizers and urea, elemental S fertilizer and the growth of legumes. Acidification causes the loss of base cations, an increase in aluminium saturation and a decline in crop yields; severe acidification can cause nonreversible clay mineral dissolution and a reduction in cation exchange capacity, accompanied by structural deterioration. Soil acidity is ameliorated by applying lime or other acid-neutralizing materials. 'Liming' also reduces N2O emissions, but this is more than offset by CO2 emissions from the lime as it neutralizes acidity. Because crop plants vary in their tolerance to acidity and plant nutrients have different optimal pH ranges, target soil pH values in the UK are set at 6.5 (5.8 in peaty soils) for cropped land and 6.0 (5.3 in peaty soils) for grassland. Agricultural lime products can be sold as 'EC Fertiliser Liming Materials' but, although vital for soil quality and agricultural production, liming tends to be strongly influenced by the economics of farming. Consequently, much less lime is being applied in the UK than required, and many arable and grassland soils are below optimum pH. Soil acidification is caused by a number of factors including acidic precipitation and the deposition from the atmosphere of acidifying gases or particles, such as sulphur dioxide, ammonia and nitric acid. The most important causes of soil acidification on agricultural land, however, are the application of ammonium-based fertilizers and urea, elemental S fertilizer and the growth of legumes. Acidification causes the loss of base cations, an increase in aluminium saturation and a decline in crop yields; severe acidification can cause nonreversible clay mineral dissolution and a reduction in cation exchange capacity, accompanied by structural deterioration. Soil acidity is ameliorated by applying lime or other acid-neutralizing materials. 'Liming' also reduces N O emissions, but this is more than offset by CO emissions from the lime as it neutralizes acidity. Because crop plants vary in their tolerance to acidity and plant nutrients have different optimal pH ranges, target soil pH values in the UK are set at 6.5 (5.8 in peaty soils) for cropped land and 6.0 (5.3 in peaty soils) for grassland. Agricultural lime products can be sold as 'EC Fertiliser Liming Materials' but, although vital for soil quality and agricultural production, liming tends to be strongly influenced by the economics of farming. Consequently, much less lime is being applied in the UK than required, and many arable and grassland soils are below optimum pH. Soil acidification is caused by a number of factors including acidic precipitation and the deposition from the atmosphere of acidifying gases or particles, such as sulphur dioxide, ammonia and nitric acid. The most important causes of soil acidification on agricultural land, however, are the application of ammonium-based fertilizers and urea, elemental S fertilizer and the growth of legumes. Acidification causes the loss of base cations, an increase in aluminium saturation and a decline in crop yields; severe acidification can cause nonreversible clay mineral dissolution and a reduction in cation exchange capacity, accompanied by structural deterioration. Soil acidity is ameliorated by applying lime or other acid-neutralizing materials. 'Liming' also reduces N2O emissions, but this is more than offset by CO 2 emissions from the lime as it neutralizes acidity. Because crop plants vary in their tolerance to acidity and plant nutrients have different optimal pH ranges, target soil pH values in the UK are set at 6.5 (5.8 in peaty soils) for cropped land and 6.0 (5.3 in peaty soils) for grassland. Agricultural lime products can be sold as 'EC Fertiliser Liming Materials' but, although vital for soil quality and agricultural production, liming tends to be strongly influenced by the economics of farming. Consequently, much less lime is being applied in the UK than required, and many arable and grassland soils are below optimum pH. Soil acidification is caused by a number of factors including acidic precipitation and the deposition from the atmosphere of acidifying gases or particles, such as sulphur dioxide, ammonia and nitric acid. The most important causes of soil acidification on agricultural land, however, are the application of ammonium‐based fertilizers and urea, elemental S fertilizer and the growth of legumes. Acidification causes the loss of base cations, an increase in aluminium saturation and a decline in crop yields; severe acidification can cause nonreversible clay mineral dissolution and a reduction in cation exchange capacity, accompanied by structural deterioration. Soil acidity is ameliorated by applying lime or other acid‐neutralizing materials. ‘Liming’ also reduces N₂O emissions, but this is more than offset by CO₂ emissions from the lime as it neutralizes acidity. Because crop plants vary in their tolerance to acidity and plant nutrients have different optimal pH ranges, target soil pH values in the UK are set at 6.5 (5.8 in peaty soils) for cropped land and 6.0 (5.3 in peaty soils) for grassland. Agricultural lime products can be sold as ‘EC Fertiliser Liming Materials’ but, although vital for soil quality and agricultural production, liming tends to be strongly influenced by the economics of farming. Consequently, much less lime is being applied in the UK than required, and many arable and grassland soils are below optimum pH. |
| Author | Goulding, K. W. T. |
| AuthorAffiliation | 1 Department of Sustainable Soils and Grassland Systems Rothamsted Research Harpenden AL5 2JQ UK |
| AuthorAffiliation_xml | – name: 1 Department of Sustainable Soils and Grassland Systems Rothamsted Research Harpenden AL5 2JQ UK |
| Author_xml | – sequence: 1 givenname: K. W. T. surname: Goulding fullname: Goulding, K. W. T. email: keith.goulding@rothamsted.ac.uk, keith.goulding@rothamsted.ac.uk organization: Department of Sustainable Soils and Grassland Systems, Rothamsted Research, AL5 2JQ, Harpenden, UK |
| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/27708478$$D View this record in MEDLINE/PubMed |
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| References | Kirkham, J.M., Rowe, B.A. & Doyle, R.B. 2007. Persistent improvements in the structure and hydraulic conductivity of a Ferrosol due to liming. Australian Journal of Soil Research, 45, 218-223. Kirkham, F.W., Tallowin, J.R.B., Sanderson, R.A., Bhogal, A., Chambers, B.J. & Stevens, D.P. 2008. The impact of organic and inorganic fertilizers and lime on the species-richness and plant functional characteristics of hay meadow communities. Biological Conservation, 141, 1411-1427. Adams F. (ed.) 1984. Soil acidity and liming, 2nd edn, Agronomy 12. American Society of Agronomy/Crop Science Society of America/Soil Science Society of America, Madison, Wisconsin. Fageria, N.K., Baligar, V.C. & Jones, C.A. 1997. Growth and mineral nutrition of field crops, 3rd edn. Marcel Dekker, New York. Kennedy, I.R. 1992. Acid soil and acid rain, 2nd edn. John Wiley and Sons, New York. Marschner, P. (ed.) 2012. Marschner's mineral nutrition of higher plants, 3rd edn. Academic Press, London. Defra. 2000. Fertiliser recommendations for agricultural and horticultural crops (RB209). TSO, London. Johnston, A.E., Goulding, K.W.T. & Poulton, P.R. 1986. Soil acidification during more than 100 years under permanent grassland and woodland at Rothamsted. Soil Use and Management, 2, 3-10. Paradelo, R., Virto, I. & Chenu, C. 2015. Net effect of liming on soil organic carbon stocks: a review. Agriculture, Ecosystems and Environment, 202, 98-107. MAFF (Ministry of Agriculture, Fisheries and Food). 1981. Lime and liming. Reference Book 35. HMSO, London. Connor, D.J., Loomis, R.J. & Cassman, K.G. 2011. Crop Ecology: productivity and Management in Agricultural Systems, 2nd edn. Cambridge University Press, Cambridge. Gibbs, P., Muir, I., Richardson, S., Hickman, G. & Chambers, B. 2005. Landspreading on agricultural land: nature and impact of paper wastes applied in England and Wales. Science Report SC030181/SR. Environment Agency, Bristol, UK. Orr, R., Murray, P., Eyles, C., Blackwell, M., Cardenas, L., Collins, A., Crawford, J., Dungait, J., Goulding, K., Griffith, B., Gurr, S., Harris, P., Hawkins, J., Misselbrook, T., Rawlings, C., Shepherd, A., Sint, H., Takahashi, T., Tozer, K., Wu, L. & Lee, M. 2016. The UK North Wyke Farm Platform: a systems approach to investigate the impact and value of temperate Grassland farming. Environmental Science and Technology, in press. Upjohn, B., Fenton, G. & Conyers, M. 2005. Soil acidity and liming. Agfact AC 19, 3rd edn. New South Wales Department of Primary Industries, Australia. Defra. 2010. The Fertiliser Manual (RB209). TSO, London. Bennett, J.McL, Greene, R.S.B., Murphy, B.W., Hocking, P. & Tongway, D. 2014. Influence of lime and gypsum on long-term rehabilitation of a Red Sodosol, in a semi-arid environment of New South Wales. Soil Research, 52, 120-128. Fornara, D.A., Steinbeiss, S., McNamara, N.P., Gleixner, G., Oakley, S., Poulton, P.R., Macdonald, A.J. & Bardgett, R.D. 2011. Increases in soil organic carbon sequestration can reduce the global warming potential of long-term liming to permanent grassland. Global Change Biology, 17, 1925-1934. Johnston, A.E. & Whinham, W.N. 1980. The use of lime on agricultural soils. Proceedings No. 189. The Fertiliser Society, Peterborough, UK. Johnston, A. E., Poulton, P. R., Dawson, C. J. & Crawley, M.J. 2001. Inputs of nutrients and lime for the maintenance of fertility of grassland soils. Proceedings No. 486. The International Fertiliser Society, York, UK. Hinsinger, P., Plassard, C., Tang, C. & Jaillard, B. 2003. Origins of root-mediated pH changes in the rhizosphere and their responses to environmental constraints: a review. Plant and Soil, 248, 43-59. GB Statutory Instruments. 1990. The Fertiliser Regulations. Statutory Instrument No. 887, HMSO, London. Goulding, K.W.T., McGrath, S.P. & Johnston, A.E. 1989. Predicting the lime requirement of soils under permanent grassland and arable crops. Soil Use and Management, 5, 54-57. Hazelton, P. & Murphy, B. 2007. Interpreting soil test results. What do all the numbers mean? CSIRO Publishing, Collingwood, Australia. Blake, L., Johnston, A.E. & Goulding, K.W.T. 1994. Mobilization of aluminium in soil by acid deposition and its uptake by grass cut for hay - a Chemical Time Bomb. Soil Use and Management, 10, 51-55. Goulding, K.W.T., Bailey, N.J., Bradbury, N.J., Hargreaves, P., Howe, M.T., Murphy, D.V., Poulton, P.R. & Willison, T.W. 1998. Nitrogen deposition and its contribution to nitrogen cycling and associated soil processes. New Phytologist, 139, 49-58. Goulding, K.W.T. & Annis, B. 1998. Lime and liming in UK agriculture. Proceedings No 410. The Fertiliser Society. York, UK. Higgins, S., Morrison, S. & Watson, C.J. 2012. Effect of annual applications of pelletized dolomitic lime on soil chemical properties and grass productivity. Soil Use and Management, 28, 62-69. Haynes, R.J. & Naidu, R. 1998. Influence of lime, fertilizer and manure applications on soil organic matter content and soil physical conditions: a review. Nutrient Cycling in Agroecosystems, 51, 123-137. Blake, L., Goulding, K.W.T., Mott, C.J.B. & Johnston, A.E. 1999. Changes in soil chemistry accompanying acidification over more than 100 years under woodland and grass at Rothamsted Experimental Station, UK. European Journal of Soil Science, 50, 401-412. Bolan, N.S., Adriano, D.C. & Curtin, D. 2003. Soil acidification and liming interactions with nutrient and heavy metal transformation and bioavailability. Advances in Agronomy, 78, 215-272. Rengel, Z. (ed.) 2003. Handbook of soil acidity. Marcel Dekker, New York. Yu, Y.-W., Fraser, M.D. & Evans, J.G. 2010. Long-term effects on sward composition and animal performance of reducing fertilizer inputs to upland permanent pasture. Grass and Forage Science, 66, 138-151. Foth, H.D. 1990. Fundamentals of soil science, 8th edn. John Wiley & Sons, New York. McGrath, S.P. & Zhao, F.J. 1995. A risk assessment of sulphur deficiency in cereals using soil and atmospheric deposition data. Soil Use and Management, 11, 110-114. Bolton, J. 1977. Changes in soil pH and exchangeable calcium in two liming experiments on contrasting soils over 12 years. Journal of Agricultural Science, 89, 81-86. Gagnon, B., Robichaud, A., Ziadi, N. & Karam, A. 2014. Repeated annual paper mill and alkaline residuals application affects soil metal fractions. Journal of Environmental Quality, 43, 517-527. Gibbons, J.M., Williamson, J.C., Williams, A.P., Withers, P.J.A., Hockley, N., Harris, I.M., Hughes, J.W., Taylor, R.L., Jones, D.L. & Healey, J.R. 2014. Sustainable nutrient management at field, farm and regional level: soil testing, nutrient budgets and the trade-off between lime application and greenhouse gas emissions. Agriculture, Ecosystems and Environment, 188, 48-56. Woodruff, C.M. 1948. Testing soils for lime requirement by means of a buffered solution and a glass electrode. Soil Science, 66, 53-63. 1989; 5 2012 2011 2010 2015; 202 1995; 11 1998 1997 2008 2007 2006 2005 2004 2003 1998; 139 1992 1977; 89 2011; 17 2008; 141 2014; 43 2003; 78 2010; 66 1986; 2 2003; 248 1990 2001 2000 1984 2016 2015 2012; 28 1981 2014 2013 1999; 50 1980 2014; 52 1948; 66 2014; 188 1998; 51 2007; 45 1994; 10 e_1_2_10_23_1 e_1_2_10_46_1 Goulding K.W.T. (e_1_2_10_22_1) 1998 e_1_2_10_24_1 e_1_2_10_45_1 Upjohn B. (e_1_2_10_47_1) 2005 Foth H.D. (e_1_2_10_16_1) 1990 e_1_2_10_44_1 e_1_2_10_43_1 e_1_2_10_42_1 e_1_2_10_20_1 Defra (e_1_2_10_13_1) 2010 Kennedy I.R. (e_1_2_10_34_1) 1992 Klein C. (e_1_2_10_30_1) 2006 GB Statutory Instruments (e_1_2_10_19_1) 1990 Marschner P. (e_1_2_10_38_1) 2012 Bolan N.S. (e_1_2_10_8_1) 2003 Johnston A. E. (e_1_2_10_33_1) 2001 e_1_2_10_2_1 Morgan M. (e_1_2_10_40_1) 2008 e_1_2_10_4_1 e_1_2_10_18_1 e_1_2_10_6_1 e_1_2_10_39_1 e_1_2_10_5_1 e_1_2_10_17_1 e_1_2_10_7_1 e_1_2_10_15_1 e_1_2_10_36_1 MAFF (Ministry of Agriculture, Fisheries and Food) (e_1_2_10_37_1) 1981 e_1_2_10_35_1 e_1_2_10_9_1 Gibbs P. (e_1_2_10_21_1) 2005 e_1_2_10_10_1 e_1_2_10_11_1 e_1_2_10_32_1 Fageria N.K. (e_1_2_10_14_1) 1997 Defra (e_1_2_10_12_1) 2000 Orr R. (e_1_2_10_41_1) 2016 Anderson G.D (e_1_2_10_3_1) 2004 Johnston A.E. (e_1_2_10_31_1) 1980 e_1_2_10_29_1 e_1_2_10_27_1 e_1_2_10_28_1 e_1_2_10_49_1 e_1_2_10_25_1 e_1_2_10_48_1 e_1_2_10_26_1 25602653 - J Environ Qual. 2014 Mar;43(2):517-27 |
| References_xml | – reference: Defra. 2000. Fertiliser recommendations for agricultural and horticultural crops (RB209). TSO, London. – reference: GB Statutory Instruments. 1990. The Fertiliser Regulations. Statutory Instrument No. 887, HMSO, London. – reference: Hazelton, P. & Murphy, B. 2007. Interpreting soil test results. What do all the numbers mean? CSIRO Publishing, Collingwood, Australia. – reference: Fageria, N.K., Baligar, V.C. & Jones, C.A. 1997. Growth and mineral nutrition of field crops, 3rd edn. Marcel Dekker, New York. – reference: Bennett, J.McL, Greene, R.S.B., Murphy, B.W., Hocking, P. & Tongway, D. 2014. Influence of lime and gypsum on long-term rehabilitation of a Red Sodosol, in a semi-arid environment of New South Wales. Soil Research, 52, 120-128. – reference: Kennedy, I.R. 1992. Acid soil and acid rain, 2nd edn. John Wiley and Sons, New York. – reference: Johnston, A.E. & Whinham, W.N. 1980. The use of lime on agricultural soils. Proceedings No. 189. The Fertiliser Society, Peterborough, UK. – reference: Goulding, K.W.T., McGrath, S.P. & Johnston, A.E. 1989. Predicting the lime requirement of soils under permanent grassland and arable crops. Soil Use and Management, 5, 54-57. – reference: Bolan, N.S., Adriano, D.C. & Curtin, D. 2003. Soil acidification and liming interactions with nutrient and heavy metal transformation and bioavailability. Advances in Agronomy, 78, 215-272. – reference: McGrath, S.P. & Zhao, F.J. 1995. A risk assessment of sulphur deficiency in cereals using soil and atmospheric deposition data. Soil Use and Management, 11, 110-114. – reference: MAFF (Ministry of Agriculture, Fisheries and Food). 1981. Lime and liming. Reference Book 35. HMSO, London. – reference: Gagnon, B., Robichaud, A., Ziadi, N. & Karam, A. 2014. Repeated annual paper mill and alkaline residuals application affects soil metal fractions. Journal of Environmental Quality, 43, 517-527. – reference: Kirkham, J.M., Rowe, B.A. & Doyle, R.B. 2007. Persistent improvements in the structure and hydraulic conductivity of a Ferrosol due to liming. Australian Journal of Soil Research, 45, 218-223. – reference: Hinsinger, P., Plassard, C., Tang, C. & Jaillard, B. 2003. Origins of root-mediated pH changes in the rhizosphere and their responses to environmental constraints: a review. Plant and Soil, 248, 43-59. – reference: Paradelo, R., Virto, I. & Chenu, C. 2015. Net effect of liming on soil organic carbon stocks: a review. Agriculture, Ecosystems and Environment, 202, 98-107. – reference: Upjohn, B., Fenton, G. & Conyers, M. 2005. Soil acidity and liming. Agfact AC 19, 3rd edn. New South Wales Department of Primary Industries, Australia. – reference: Adams F. (ed.) 1984. Soil acidity and liming, 2nd edn, Agronomy 12. American Society of Agronomy/Crop Science Society of America/Soil Science Society of America, Madison, Wisconsin. – reference: Orr, R., Murray, P., Eyles, C., Blackwell, M., Cardenas, L., Collins, A., Crawford, J., Dungait, J., Goulding, K., Griffith, B., Gurr, S., Harris, P., Hawkins, J., Misselbrook, T., Rawlings, C., Shepherd, A., Sint, H., Takahashi, T., Tozer, K., Wu, L. & Lee, M. 2016. The UK North Wyke Farm Platform: a systems approach to investigate the impact and value of temperate Grassland farming. Environmental Science and Technology, in press. – reference: Fornara, D.A., Steinbeiss, S., McNamara, N.P., Gleixner, G., Oakley, S., Poulton, P.R., Macdonald, A.J. & Bardgett, R.D. 2011. Increases in soil organic carbon sequestration can reduce the global warming potential of long-term liming to permanent grassland. Global Change Biology, 17, 1925-1934. – reference: Defra. 2010. The Fertiliser Manual (RB209). TSO, London. – reference: Blake, L., Johnston, A.E. & Goulding, K.W.T. 1994. Mobilization of aluminium in soil by acid deposition and its uptake by grass cut for hay - a Chemical Time Bomb. Soil Use and Management, 10, 51-55. – reference: Haynes, R.J. & Naidu, R. 1998. Influence of lime, fertilizer and manure applications on soil organic matter content and soil physical conditions: a review. Nutrient Cycling in Agroecosystems, 51, 123-137. – reference: Goulding, K.W.T., Bailey, N.J., Bradbury, N.J., Hargreaves, P., Howe, M.T., Murphy, D.V., Poulton, P.R. & Willison, T.W. 1998. Nitrogen deposition and its contribution to nitrogen cycling and associated soil processes. New Phytologist, 139, 49-58. – reference: Rengel, Z. (ed.) 2003. Handbook of soil acidity. Marcel Dekker, New York. – reference: Higgins, S., Morrison, S. & Watson, C.J. 2012. Effect of annual applications of pelletized dolomitic lime on soil chemical properties and grass productivity. Soil Use and Management, 28, 62-69. – reference: Johnston, A.E., Goulding, K.W.T. & Poulton, P.R. 1986. Soil acidification during more than 100 years under permanent grassland and woodland at Rothamsted. Soil Use and Management, 2, 3-10. – reference: Johnston, A. E., Poulton, P. R., Dawson, C. J. & Crawley, M.J. 2001. Inputs of nutrients and lime for the maintenance of fertility of grassland soils. Proceedings No. 486. The International Fertiliser Society, York, UK. – reference: Woodruff, C.M. 1948. Testing soils for lime requirement by means of a buffered solution and a glass electrode. Soil Science, 66, 53-63. – reference: Blake, L., Goulding, K.W.T., Mott, C.J.B. & Johnston, A.E. 1999. Changes in soil chemistry accompanying acidification over more than 100 years under woodland and grass at Rothamsted Experimental Station, UK. European Journal of Soil Science, 50, 401-412. – reference: Foth, H.D. 1990. Fundamentals of soil science, 8th edn. John Wiley & Sons, New York. – reference: Marschner, P. (ed.) 2012. Marschner's mineral nutrition of higher plants, 3rd edn. Academic Press, London. – reference: Gibbons, J.M., Williamson, J.C., Williams, A.P., Withers, P.J.A., Hockley, N., Harris, I.M., Hughes, J.W., Taylor, R.L., Jones, D.L. & Healey, J.R. 2014. Sustainable nutrient management at field, farm and regional level: soil testing, nutrient budgets and the trade-off between lime application and greenhouse gas emissions. Agriculture, Ecosystems and Environment, 188, 48-56. – reference: Bolton, J. 1977. Changes in soil pH and exchangeable calcium in two liming experiments on contrasting soils over 12 years. Journal of Agricultural Science, 89, 81-86. – reference: Goulding, K.W.T. & Annis, B. 1998. Lime and liming in UK agriculture. Proceedings No 410. The Fertiliser Society. York, UK. – reference: Kirkham, F.W., Tallowin, J.R.B., Sanderson, R.A., Bhogal, A., Chambers, B.J. & Stevens, D.P. 2008. The impact of organic and inorganic fertilizers and lime on the species-richness and plant functional characteristics of hay meadow communities. Biological Conservation, 141, 1411-1427. – reference: Gibbs, P., Muir, I., Richardson, S., Hickman, G. & Chambers, B. 2005. Landspreading on agricultural land: nature and impact of paper wastes applied in England and Wales. Science Report SC030181/SR. Environment Agency, Bristol, UK. – reference: Yu, Y.-W., Fraser, M.D. & Evans, J.G. 2010. Long-term effects on sward composition and animal performance of reducing fertilizer inputs to upland permanent pasture. Grass and Forage Science, 66, 138-151. – reference: Connor, D.J., Loomis, R.J. & Cassman, K.G. 2011. Crop Ecology: productivity and Management in Agricultural Systems, 2nd edn. Cambridge University Press, Cambridge. – year: 2011 – volume: 43 start-page: 517 year: 2014 end-page: 527 article-title: Repeated annual paper mill and alkaline residuals application affects soil metal fractions publication-title: Journal of Environmental Quality – volume: 248 start-page: 43 year: 2003 end-page: 59 article-title: Origins of root‐mediated pH changes in the rhizosphere and their responses to environmental constraints: a review publication-title: Plant and Soil – start-page: 992 year: 2008 end-page: 4 – volume: 188 start-page: 48 year: 2014 end-page: 56 article-title: Sustainable nutrient management at field, farm and regional level: soil testing, nutrient budgets and the trade‐off between lime application and greenhouse gas emissions publication-title: Agriculture, Ecosystems and Environment – year: 1981 – year: 2005 – volume: 28 start-page: 62 year: 2012 end-page: 69 article-title: Effect of annual applications of pelletized dolomitic lime on soil chemical properties and grass productivity publication-title: Soil Use and Management – volume: 2 start-page: 3 year: 1986 end-page: 10 article-title: Soil acidification during more than 100 years under permanent grassland and woodland at Rothamsted publication-title: Soil Use and Management – volume: 17 start-page: 1925 year: 2011 end-page: 1934 article-title: Increases in soil organic carbon sequestration can reduce the global warming potential of long‐term liming to permanent grassland publication-title: Global Change Biology – year: 2007 – year: 2001 – volume: 78 start-page: 215 year: 2003 end-page: 272 article-title: Soil acidification and liming interactions with nutrient and heavy metal transformation and bioavailability publication-title: Advances in Agronomy – volume: 11 start-page: 110 year: 1995 end-page: 114 article-title: A risk assessment of sulphur deficiency in cereals using soil and atmospheric deposition data publication-title: Soil Use and Management – year: 2003 – year: 2000 – start-page: 96 year: 2004 end-page: 100 – volume: 45 start-page: 218 year: 2007 end-page: 223 article-title: Persistent improvements in the structure and hydraulic conductivity of a Ferrosol due to liming publication-title: Australian Journal of Soil Research – volume: 139 start-page: 49 year: 1998 end-page: 58 article-title: Nitrogen deposition and its contribution to nitrogen cycling and associated soil processes publication-title: New Phytologist – start-page: 29 year: 2003 end-page: 52 – volume: 10 start-page: 51 year: 1994 end-page: 55 article-title: Mobilization of aluminium in soil by acid deposition and its uptake by grass cut for hay ‐ a Chemical Time Bomb publication-title: Soil Use and Management – year: 1990 – year: 1992 – volume: 89 start-page: 81 year: 1977 end-page: 86 article-title: Changes in soil pH and exchangeable calcium in two liming experiments on contrasting soils over 12 years publication-title: Journal of Agricultural Science – year: 2014 – volume: 51 start-page: 123 year: 1998 end-page: 137 article-title: Influence of lime, fertilizer and manure applications on soil organic matter content and soil physical conditions: a review publication-title: Nutrient Cycling in Agroecosystems – year: 2010 – year: 1998 – volume: 5 start-page: 54 year: 1989 end-page: 57 article-title: Predicting the lime requirement of soils under permanent grassland and arable crops publication-title: Soil Use and Management – year: 2012 – volume: 66 start-page: 138 year: 2010 end-page: 151 article-title: Long‐term effects on sward composition and animal performance of reducing fertilizer inputs to upland permanent pasture publication-title: Grass and Forage Science – volume: 52 start-page: 120 year: 2014 end-page: 128 article-title: Influence of lime and gypsum on long‐term rehabilitation of a Red Sodosol, in a semi‐arid environment of New South Wales publication-title: Soil Research – year: 1984 – volume: 66 start-page: 53 year: 1948 end-page: 63 article-title: Testing soils for lime requirement by means of a buffered solution and a glass electrode publication-title: Soil Science – year: 2016 article-title: The UK North Wyke Farm Platform: a systems approach to investigate the impact and value of temperate Grassland farming publication-title: Environmental Science and Technology – start-page: 294 year: 2012 – year: 1980 – year: 2006 – volume: 141 start-page: 1411 year: 2008 end-page: 1427 article-title: The impact of organic and inorganic fertilizers and lime on the species‐richness and plant functional characteristics of hay meadow communities publication-title: Biological Conservation – year: 1997 – volume: 202 start-page: 98 year: 2015 end-page: 107 article-title: Net effect of liming on soil organic carbon stocks: a review publication-title: Agriculture, Ecosystems and Environment – year: 2015 – year: 2013 – volume: 50 start-page: 401 year: 1999 end-page: 412 article-title: Changes in soil chemistry accompanying acidification over more than 100 years under woodland and grass at Rothamsted Experimental Station, UK publication-title: European Journal of Soil Science – volume-title: Landspreading on agricultural land: nature and impact of paper wastes applied in England and Wales. 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| SubjectTerms | Acid deposition Acidification Acidity Agricultural land Agricultural production agricultural soils Aluminum ammonia Ammonium carbon dioxide Carbon dioxide emissions Cation exchange cation exchange capacity Cation exchanging Cations chemical bases clay Crop yield crops Farming farming systems Farms fertilizer Fertilizers gases grassland soils Grasslands greenhouse gas emissions Land legumes Lime lime requirement Liming liming materials neutralization Nitric acid Nitrous oxide nutrients Review Soil (material) Soil acidification Soil pH Soil Physico‐chemical Properties and Their Management Soil quality Soils Sulfur dioxide sulfur fertilizers United Kingdom Urea urea fertilizers |
| Title | Soil acidification and the importance of liming agricultural soils with particular reference to the United Kingdom |
| URI | https://api.istex.fr/ark:/67375/WNG-XK974WZ5-6/fulltext.pdf https://onlinelibrary.wiley.com/doi/abs/10.1111%2Fsum.12270 https://www.ncbi.nlm.nih.gov/pubmed/27708478 https://www.proquest.com/docview/1816818366 https://www.proquest.com/docview/1827908042 https://www.proquest.com/docview/1835373852 https://www.proquest.com/docview/1835608965 https://www.proquest.com/docview/2000107594 https://pubmed.ncbi.nlm.nih.gov/PMC5032897 |
| Volume | 32 |
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