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Removal of Boron from Well Waters for Irrigation of Agricultural Lands

机译:从水域中除去硼,用于农业土地灌溉

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Boron is widely distributed in both the hydrosphere and lithosphere of the earth (Morgan, 1980). This element is one of the seven essential micronutrients required for the normal growth of most plants. However, Boron if present in excessive amounts may cause problems of toxicity. There is a relatively small range between levels of soil boron causing deficiency and toxicity symptoms in plants (Keren and Bingham, 1985). In the recent years, a significant increase in the concentration of boron in surface and ground waters has been observed, limiting the use of water for crop irrigation. Values between 1.0 and 4.0 ig of B/mL of water produce cellular necrosis, affecting the biological functioning and yields of crops (Vazquez et al., 2011). Before usingthis water for irrigation of agricultural areas, especially in soils with already limiting physicochemical conditions, a treatment to remove boron and other associated problems is necessary. The use of Diammonium phosphate (NH4)2P04 and Calcium hydroxide Ca(OH)2 in the removal of boron, through the formation of hydroxyapatite (HAp), was evaluated. In addition, the effect of two flocculants (calcium sulphate (CaS04.2H20) and aluminum sulphate (Ab(S04)3) at concentrations of 35% w/v to accelerate the precipitation of calcium borate hydroxide, resulting from the formation of HAp, was studied. Boron removal started to occur at 30 minutes of the reaction time, after Ca(OH)2 + (NHO2HPO4 were added. Additional removal of boron was obtained when flocculants were added, especially when gypsum was used. Boron concentration was reduced from 18 ppm to about 8.5 ppm after 30 minutes and to about 3 ppm after 4 hours (Figure 1), corresponding to a removal of about 80% as compared to the initial concentration. For smaller initial concentrations (5 ug of B/mL) B content was lowered to about 0.98 ug of B/mL. The results indicated that the use of Ca(OH)2 + (NH4)2HPCm in addition to the use of gypsum (CaS04.2H20) at 35 % w/v) is an alternative to treat water and removeboron to values acceptable for crop irrigation. However, pH also needs to be adjusted before a recommendation can be made. After the removal process, the pH of the solution was about 11.5 and adjustment was needed to lower the pH to values acceptable for crop production.
机译:硼广泛分布在地球的水圈和岩石圈(Morgan,1980)中。该元素是大多数植物正常生长所需的七种必需的微量营养素之一。然而,硼如果存在过量的量可能会导致毒性问题。在土壤硼水平之间导致植物缺乏和毒性症状之间存在相对较小的范围(Keren和Bingham,1985)。近年来,已经观察到表面和地面水中硼浓度的显着增加,限制了使用水进行作物灌溉。 1.0和4.0 Ig的值B / ml水产生细胞坏死,影响作物的生物功能和产量(Vazquez等,2011)。在使用该水域的农业区域灌溉之前,特别是在具有限制物理化学条件的土壤中,需要去除硼和其他相关问题的治疗。评价在通过形成羟基磷灰石(HAP)中除去硼的磷酸铵(NH 4)2P04和氢氧化钙Ca(OH)2中的使用。此外,两种絮凝剂(硫酸钙(Cas04.2H20)和硫酸铝(SO 4)3)的效果在35%w / v的浓度下加速氢氧化钙的沉淀,由Hap的形成产生,研究了。在加入Ca(OH)2 +(加入NHO2HPO 4后,在反应时间的30分钟开始发生硼。当加入絮凝剂时,尤其是当使用石膏时,从而降低了硼。硼浓度降低在30分钟后18ppm至约8.5ppm,4小时后约3ppm(图1),与初始浓度相比,除去约80%。对于较小的初始浓度(5μgb/ ml)b含量降至约0.98μg的B / ml。结果表明除了使用石膏(Cas04.2h20)的使用,Ca(OH)2 +(NH 4)2HPCM在35%w / v)是一个替代物,将水和删除鳄鱼治疗到作物灌溉可接受的值。但是,pH也需要遵守在可以提出建议之前删除。在去除过程之后,溶液的pH约为11.5,需要调节以将pH降低到作物生产可接受的值。

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