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Solubility and Leaching of Boron from Borax and Colemanite in Flooded Acidic Soils

机译:酸性土壤中硼砂和硬锰矿中硼的溶解度和溶出

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Boron (B) is a micronutrient essential for adequate plant growth. Borax (Na2B4O7 center dot 10H2O) and colemanite (Ca2B6O11 center dot 5H2O) are common B fertilizer materials, the former being widely used worldwide. Boron is completely water soluble and subjected to leaching. In this study, the dissolution kinetics of both borax and colemanite in deionized water and at pH 3.8, 5.2, 6.5, and 8.2 were determined. Soils incubated with minerals for 40 days and 80 pore volumes of leachates from repacked soil column treated with either surface-applied borax or colemanite (powdered and granular) were collected and analyzed for B contents. Two different soils, Chempaka (Typic paleudult) and Tepus (Typic Kandiaquult) series, taken from paddy-growing areas were used in leaching and incubation studies. Dissolution rate of borax was greater than that of colemanite, and complete dissolution was observed after 100 min, whereas complete dissolution of colemanite was not reached even after 300 min. There was no effect of pH on dissolution rate of borax and colemanite. Boron released from borax was hasty, and after 5 weeks no more B was released. In the case of colemanite, B released was steadily increased until the end of the incubation study. At the end of the study, there was no significant difference in B levels of both borax- and colemanite-applied soils. Particle size had a significant effect on the solubility and dissolution rate of colemanite. Boron dissolution rate and solubility from colemanite powder were significantly greater than those from granular colemanite. Leaching losses from borax were much greater than from colemanite as indicated by the breakthrough curves, which were earlier for borax than colemanite. After 60 pore volumes, no more B was leached out from borax, and in the leachates of colemanite some concentration was detected even after 80 pore volumes. Boron content in soil of columns after the completion of the experiment was greater in case of colemanite. Borax and colemanite fertilizers showed the same trend of leaching and B releasing in both Tepus and Chempaka soil series.
机译:硼(B)是微量元素,对植物的正常生长至关重要。硼砂(Na2B4O7中心点10H2O)和硬锰矿(Ca2B6O11中心点5H2O)是常见的B肥材料,前者在世界范围内广泛使用。硼是完全水溶性的,并经过浸出。在这项研究中,测定了硼砂和硬锰矿在去离子水中以及pH值3.8、5.2、6.5和8.2时的溶解动力学。收集了与矿物一起孵育40天的土壤,以及用表面处理的硼砂或硬锰矿(粉状和粒状)处理过的重装土壤柱中80孔体积的渗滤液,并对其B含量进行了分析。从稻田中获取的两种不同土壤,Chempaka(典型的palududult)和Tepus(典型的Kandiaquult)系列被用于淋洗和孵化研究。硼砂的溶出速率大于硬锰矿,并且在100分钟后观察到完全溶出,而即使在300分钟后也未达到硬锰矿的完全溶出。 pH值对硼砂和硬锰矿的溶解速率没有影响。从硼砂中释放出来的硼很仓促,在5周后不再释放出B。对于硬锰矿,释放的B稳定增加,直到温育研究结束。在研究结束时,硼砂和硬锰矿施用土壤的B水平均无显着差异。粒度对硬锰矿的溶解度和溶解速率有显着影响。来自硬锰矿粉的硼溶解速率和溶解度显着大于颗粒状硬锰矿的硼溶解速率和溶解度。穿透曲线表明,硼砂的浸出损失比钴锰矿的浸出损失大得多,而硼砂的浸出损失早于钴锰矿。经过60个孔体积后,硼砂中不再有B浸出,甚至在80个孔体积后,在堇青石的浸出液中也检测到一些浓度。实验完成后,如果是硬锰矿,则柱中土壤中的硼含量更高。硼砂和硬锰矿肥在Tepus和Chempaka土壤系列中均表现出相同的浸出和B释放趋势。

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