Effect of Different Magnesium Concentration inWater on Soil Characteristics and Determining the Critical Concentration

Document Type : Research Paper

Authors

Abstract

Usually, the impact of calcium and magnesium on improving and maintaining soil structure is
assumed to be similar. This study was conducted to investigate the effect of different concentrations
of magnesium on soil quality indicators. A clay loam soil was treated with four concentrations of
magnesium (0, 1, 2, 3, 4, and 5 mmol/L) during 4 months in a completely randomized design with
three replications. After this period, the mean weight diameter(MWD), wet aggregate
stability(WAS) , clay dispersion (DS) and soil saturated hydraulic conductivity(KS )were measured.
Analysis of variances showed that aggregate stability, hydraulic conductivity and clay dispersion
significantly (p<0.01) were affected by different magnesium concentrations. By 3 mmol/L of
magnesium wet aggregate stability and hydraulic conductivity increased due to substitution of the
sodium by magnesium which resulted in clay dispersion reduction. Substitution of the calcium by
magnesium in concentrations more than 3 mmol/L resulted in lower aggregate stabilities due to
special features of the magnesium such as higher hydrated radius and hydration energy compared to
the calcium.

Keywords

Main Subjects


منابعمورداستفاده
تاجیک ف،1383. ارزیابی پایداری خاکدانه در برخی مناطق ایران. مجله علوم و فنون کشاورزی و منابع طبیعی، سال 8، شماره 1، صفحه­های 107 تا 122.
علیزاده ا، 1385. رابطه آب، خاک و گیاه. انتشارات دانشگاه فردوسی، مشهد.
Adesodun JK, Mbagwu JSC and Oti N, 2005. Distribution of carbon, nitrogen and phosphorus in water-stable aggregates of an organic waste amended Ultisol in southern Nigeria. Bioresource Technology 96(4): 509-516.
Agar AI, 2012. Improvement of exchangeable Ca:Mg ratio by using gypsum and waste of sulfur in   magnesium-affected soils. African Journal of Agricultural Research 7(14): 2205-2214.
Agassi M, 1996. Soil Erosion, Conservation and Rehabilitation. New York: Marcell Dekker.
Armstrong ASB and Tanton TW, 1992. Gypsum applications to aggregated saline sodic clay topsoils. Journal of Soil Science 43: 249-260.
Basaka SK, Chaudhariab D and Sharmaa K, 2015. Impact of varying Ca/Mg waters on ionic balance, dispersion, and clay flocculation of salt-affected soils. Communications in soil Science and plant analysis 46: 827-844.
Bekbaev R, Vyshpolsky F, Ibatullin S, Mukhamedjanov Kh and Bekbaev U, 2005. Influence of application of phosphogypsum on infiltration rate of solonetzic soil. Bull agriculture Science. kazakhstan (in Russian) 7: 18-20.
Ben-Hur M, Shainberg I, Bakker D and Keren R, 1985. Effect of soil texture and CaCO3 content on water infiltration in crusted soil as related to water salinity. Irrigation Science 6: 281-294.
Boix-Fayos C, Calvo-Cases A and Imeson AC, 2001. Influence of soil properties on the aggregation of some mediterranean soils and the use of aggregate size and stability as land degradation indicators. Catena 44: 47-67.
Bronick CJ and Lal R, 2005. Soil structure and management: a review. Geoderma 124: 3-22.
Chan KY and Heenan DP, 1999. Lime-induced loss of soil organic carbon and effect on aggregate stability. Soil Science Society of America Journal 63: 1841-1844.
Dextor Ar and Chan KY, 1991. Soils mechanical properties as influenced by exchangeable cations. Journal of Soil Science 42: 219-226.
Dontsova KM and Norton LD, 2002. Clay dispersion, infiltration and erosion as influenced by exchangeable Ca and Mg. Journal of Soil Science 167: 184-193.
Donstova KM, Norton D, Jonston C and Bigham J, 2004. Influence of exchangeable cations on water adsorption by soil clays. american journal of soil science society 68:1218-1227.
Hadas A and Frenkel H, 1982. Infiltration as affected by long-term use of sodic-saline water for
Irrigation. Soil Science Society of America Journal 46: 524-530.
Igwe CA and Udegbunam ON, 2008. Soil properties influencing water-dispersible clay and silt in
         an ultisol in southern Nigeria. International Agrophysics 22: 319-325.
Karajeh F, Karimov A, Mukhamedjanov V, Vyshpolsky F, Mukhamedjanov Kh, Ikramov R, Palvanov T and Novikova A, 2004. Improved on-farm water management strategies in central Asia. In: Ryan J, Vlek P and Paroda R (eds). Agriculture in central asia research for development. ICARDA, Aleppo, Syria, and center for development research, Bonn, Germany 76-89.
Karimov A, Qadir M, Noble A, Vyshpolsky F and Anzelm K, 2009. The development of magnesium-dominant soils under irrigated agriculture in southern Kazakhstan. Pedosphere 19: 331-343.
Kemper WD and Rosenau RC, 1986. Aggregate stability and size distribution. pp: 425-442.
Klute A, 1986. Methods of soil analysis. Part 1: Physical and microbiological methods, second edition. american society of agronomy, Inc. soil science society of america, Inc. publisher madison, wisconsin.
Lado M, Paz A, and Ben-Hur M, 2004. Organic matter and aggregate-size interactions in saturated hydraulic conductivity. american journal of soil science society 68:234-242.
Lebron I, Suarez DL and Yoshida T, 2002. Gypsum effect on the aggregate size and geometry of three sodic soils under reclamation. american journal of soil science society 66: 92-98.
Levy GJ and Torrento JR, 1995. Clay dispersion and macro aggregate stability as affected by exchangeable K and Sodium. Journal of soil science 160: 352–358.
Mamedov A and Levy GJ, 2001. Clay dispersivity and aggregate stability effects on seal formation and erosion in effluent–irrigated soils. Journal of soil science 166(9):631-639.
Martinez J, 1999. Irrigation with saline water. Agricultural Water Management 40: 183-194.       
Neaman A and Singer A, 2004. The effects of palygorskite on chemical and physicochemical properties of soils: A review. Geoderma 123(3): 297-303.
Orts JW, Sojka RE and Glenn GM, 2000. Biopolymer additives to reduce erosion induced soil losses during irrigation. Industrial Crops and Products 11: 19-26.
Ogbonna C.S, Igwe C.A and Ogbonna P, 2013. Effects of exchangeable Ca:Mg ratio on the dispersion of soils some southern Nigeria soils. Agro science 2: 10-19.
Page A. L, 1983. Methods of soil analysis. Part 2: Chemical and microbiological properties (Agronomy), 2 sub edition. ameer society of agronomy.
Pojasok T and kay BD, 1990. Assessment of combination of wet sieving and turbidimetry to characterize the structural stability of moist aggregate. Canadian Journal of soil science 70: 33-42.
Qadir M and Schubert S, 2002. Degradation processes and nutrient constraints in sodic soils. Land degrad 13:275-294.
Shainberg I and Letey J, 1984. Response of soils to sodic and saline conditions. Hilgardia 52: 1-57.
Shainberg I Alperovitch N and Keren R, 1988. Effect of magnesium on the hydraulic conductivity of Na-smectite-sand mixtures. Clays and clay minerals 36(5): 432-438.
Six J, Feller C, Denef K, Oglen SM, Moraes JC, and Albrecht A, 2002. Soil organic matter, biot and aggregation in temperate and tropical soils-effect of no tillage. Agron 22: 755-775.
Spaccini R, Zena A, Igwe CA, Mbagwu JSC and Picolla A, 2001. Carbohydrate in water stable aggregates and particle size fractions in forested and cultivated soils in two contrasting tropical ecosystems. Biogeochemistry 53: 1-22.
Turkoza M, Savasa H, Acaza A and Tosunb H, 2014. The effect of magnesium chloride solution on the engineering properties of clay soil with expansive and dispersive characteristics. Applied clay science 101:1-9.
US Salinity Laboratory Staff, 1954. Diagnosis and important of saline and alkali soils. USDA Handbook 60. US Gov. Print Ofiice, Washington, DC.
Vyshpolsky F, Qadir M, Karimov A, Mukhamedjanov K, Bekbaev U, Paroda R, Aw-Hassan A and Karajeh F, 2008. Enhancing the productivity of high-magnesium soil and water resources through the application of phosphogypsum in central Asia. Land degrad 19: 45-56.
Zhang XC and Norton LD, 2002. Effect of exchangeable Mg on saturated hydraulic conductivity,disaggregation and clay dispersion of disturbed soils. Journal of Hydrology 260: 194-205.