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Zeolites as Micro-Pore System and Their Usage Prospects

机译:沸石作为微孔系统及其使用前景

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Zeolites belong to the natural rock the constant usage of which in science and practice has the following basis: its high ion-exchanging capacity, prolonged activity of water and salt changing mode in soil (after effect); selectivity towards NH_4~+ and K~+, which causes increasing the coefficient of their usage by plants and enhancing efficacy of mineral fertilizers. Taking growing dosages (3-6-9-12 T/Hectares) of zeolites in red soils of West Georgia at the background of mineral fertilizers (NPK) caused increasing of P, K, Ca, Mg in tea leaves. Nitrogen decreasing tendency must be caused by selective absorption of NH_4~+ by zeolites, which increases nitrogen usage coefficient by tea plant. Taking zeolites in the red soils with mineral fertilizers improves tea leave quality. Compared to the background option usage of zeolites by 12 tonnes/hectare dosage, caused increasing tannin and extractive substances by 3.8-3.3%. Zeolites improve physical-chemical properties of the soil, in particular: strong acid reaction of red soils was decreased up to pH 4.5-5.8, it was caused by increasing Calcium and Magnesium easily soluble in water, which caused increasing pH of soil. By taking 12 tonnes/hectare zeolites in soils P_2O_5 and K_2O concentration increase is indicated (P_2O_5 -78.5 mg/100 g; K_2O - 14.6 mg/100 g) as well as hummus (4.22%) and total nitrogen consistency (0.29%) was increased in soils.
机译:沸石属于天然岩石,在科学和实践中的持续用法具有以下基础:其高离子交换能力,延长水和土壤中的盐变化模式(效果后);选择性朝向NH_4〜+和K +,导致植物使用的使用系数和提高矿物肥料的疗效。在矿物肥料(NPK)背景下,在西格鲁吉亚西格鲁吉亚的红色土壤中吞吐量(3-6-6-12吨/公顷)引起茶叶中的P,K,Ca,Mg增加。氮气递减趋势必须是由沸石的选择性吸收引起的,这增加了茶厂的氮使用系数。在用矿物肥料的红壤中服用沸石改善了茶叶质量。与沸石的背景选择相比,沸石12吨/公顷的剂量,使单宁和萃取物质增加3.8-3.3%。沸石改善了土壤的物理化学性质,特别是:红色土壤的强酸反应降低至pH4.5-5.8,是由增加钙和镁易溶于水的钙和镁引起的土壤。通过在土壤中服用12吨/公顷的沸石P_2O_5和K_2O浓度增加(P_2O_5 -78.5mg / 100g; K_2O -14.6mg / 100g / 100g)以及Hummus(4.22%)和总氮一致性(0.29%)在土壤中增加。

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