آزاد سازی منیزیم از کانی سپیولیت تحت تاثیر دو اسید آلی

[1] Rasmussen R.A., Borggaard O.K., Hansen H.C.B., Olsson M., “Effect of natural organic soil solutes on weathering rates of soil minerals”, Soil Science 49 (1998) 397-406.

[2] Marschner H., “Mineral nutrition of higher plants”. Academic Press. London (1995).

[3] Wang J.G., Zhang, F.S., Zhang X.L., Cao Y.P., “Release of potassium from K-bearing minerals: effect of plant roots under P deficiency”, Nutrient Cycling in Agroecosystems 56 (2000) 45-52

[4] Jones D. L., Darrah P. R., “Influx and efflux of organic-acids across the soil-root interface of Zea mays L. and its implications in rhizosphere C flow”, Plant and Soil 173 (1995) 103-109.

[5] Strobel W., “Influence of vegetation on low molecular-weight carboxylic acids in soil solution, A review”, Geoderma 99 (2001) 169-198.

[6] Sposito G., “The chemistry of soil”. Oxford. University Press. New York (1989).

[7] Hinsinger P., Elsass, F., Jaillard B., Robert M., “Root-induced irreversible transformation of trioctahedral mica in the rhizosphere of rape”, Soil Science 44 (1993) 535-545.

[8] Tu S. X., Guo Z. F., Sun. J. H., “Effect of oxalic acid on potassium release from typical Chinese soils and Minerals”, Pedosphere 17(2007) 1-10.

[9] Kodama H., Schnitzer M., Jaakkimainen M., “Chlorite and biotite weathering by fulvic acid solutions in closed and open systems”, Canadian Journal of Soil Science 63 (1983) 619-629.

[10] Huang W.H., Keller W.D., “Dissolution of rock-forming silicate minerals in organic acids: Simulated first stage weathering of fresh mineral”, American mineralogists 55 (1970) 2076-2094.

[11] Stumm W., Furrer G., Kunz B., “The role of surface coordination in precipitation and dissolution of mineral surfaces”, Croatica Chemica Acta 56 (1983) 593-611.

[12] Singer A., “Palygorskite and sepiolite group minerals”. In: Dixon, J.B. and S.B. Weed (Eds.), Minerals in soil Environments. Soil Science Society of America, Madison, WI, (1989) 829-872.

[13] Serratosa J.M., “Surface properties of fibrous clay minerals (palygorskite and sepiolite”. In: Mortland, M .M., Farmer V .C., (Eds.), Proceeding of International Clay Conference (1979).

[14] Russel E. W., “Soil Conditions and Plant Growth”. Longman. London (1961) 1014 p.

[15] Carter D. L., Mortland M.M., Kemper, W.D., “Specific surface”. In: Klute, A. (ed.), Methods of Soil Analysis Part 1: Physical and Mineralogical Methods. Soil Science Society of America and American Society of Agronomy, Madison, WI, (1996) pp. 413-423.

[16] نوروزی س.، خادمی ح.، “آزادسازی پتاسیم از موسکویت و فلوگوپیت توسط چند اسید آلی”، مجله آب و خاک، شماره 23 (1388) ص 273-263.

[17] Singer A., Stahr K., Zarei M.,”Characteristics and origin of sepiolite (Meerschaum) from Central Somalia”, Clay Minerals 33 (1998) 349-362.

[18] Pohlman A.A., McColl J., “Kinetics of metal dissolution from forest soil by soluble organic Acids”. Journal of Environmental Quality 15 (1986) 86-92.

[19] بحرینی طوحان م.، دردی پور ا.، موحدی نایینی س، ع.، “سرعت رهاسازی پتاسیم غیر تبادلی با استفاده از اسید سیتریک و کلرید کلسیم رقیق در خاک‌های زراعی سری‌های غالب استان گلستان”، مجله علوم و فنون کشاورزی و منابع طبیعی، مجله علوم آب و خاک، شماره 14(1389) ص 126-113.

[20] Jones D. L., “Organic Acids in the rhizosphere -A critical review”, Plant and Soil 205 (1998) 25- 44.

[21] Albert, A., Serjean E.P., “The Determination of Ionization Constants”, Third, Edition Chapman and Hall, London (1984).

[22] Drever, J. I., Stillings L. L., “The role of organic acids in mineral weathering”, Colloids and Surfaces, A: Physicochemical and Engineering Aspects 120 (1997)167-181.

[23] Zhang H., Bloom P. R. “Dissolution kinetics of hornblende in organic acid solution”, Soil Science Society of America Journal 63 (1999) 815-822.

[24] Bolan, N.S., Naidu R., Mahimairaja, S., Baskaran S., “Influence of low-molecular-weight organic-acids on the solubilization of phosphates”, Biology and Fertility of Soils 18 (1994) 311-319.

[25] Manley E. P., Evans L. J., ”Dissolution of feldspars by low molecular weight aliphatic and aromatic acids”. Soil Scienc 141 (1986) 106-112.

[26] Miura A., Nakazawa K, Takei T., Kumada N., Kinomura N., Ohki R., Koshiyama H.,”Acid, base, and heat induced degradation behavior of Chinese sepiolite”, Ceramics International 38 (2012) 4677– 4684.

[27] Giustetto R., Wahyudi, O., Corazzari I., Turc F.,”Chemical stability and dehydration behavior of a sepiolite/indigo Maya Blue pigment”, Applied Clay Science 52 (2011) 41–50.

[28] Ozdemir M., , Kipcak I.”Dissolution kinetics of sepiolite in hydrochloric acid and nitric acid”, Clay and Clay Minerals 6 (2004) 714-720.

[29] Boyle J. R., Voigt G. K., Sawhney B. L., “Chemical weathering of biotite by organic acids”, Soil Science 117(1974) 42-45.

[30] Chin P.K.F., Mills G. L., “Kinetics and mechanisms of kaolinite dissolution: effects of organic ligands”, Chemical Geology 90 (1991) 307-317.

[31] Cubillo A.E., Zapardiel R.P., Moya J.S., Barba M.F., Pecharroman C., “The role of magnesium on the stability of crystalline sepiolte structure”, Ceramic Society 28 (2008) 1763-1768.

[32] Reitemeire R.F. “The chemistry of soil potassium”, Advances in Agronomy 3 (1951) 113-164.

[33] حاتمی م.، کریمی .، ع ر.، فتوت ا.، خادمی ح.، ″بررسی تأثیر اندازه ذرات و نوع عصاره گیر بر شکل‌های مختلف پتاسیم برخی کانی های میکایی و فلدسپات پتاسیم”، مجله پژوهش های حفاظت آب و خاک، شماره20 (1392) ص 115-132.

[34] Snall S., Liljefors T., “Leachability of major elements from minerals in strong acids”, Journal of Geochemical Exploration 71 (2000) 1-12.