毛敬麟, 刘可星, 何慧中, 郭小雪, 廖宗文. 活化剂对富钾页岩、钾长石的活化效果及作用机理[J]. 华南农业大学学报, 2015, 36(1): 60-64. DOI: 10.7671/j.issn.1001-411X.2015.01.011
    引用本文: 毛敬麟, 刘可星, 何慧中, 郭小雪, 廖宗文. 活化剂对富钾页岩、钾长石的活化效果及作用机理[J]. 华南农业大学学报, 2015, 36(1): 60-64. DOI: 10.7671/j.issn.1001-411X.2015.01.011
    MAO Jinglin, LIU Kexing, HE Huizhong, GUO Xiaoxue, LIAO Zongwen. Effects of the activator on potassium release from potassium-rich shale and potassium feldspar and its mechanism[J]. Journal of South China Agricultural University, 2015, 36(1): 60-64. DOI: 10.7671/j.issn.1001-411X.2015.01.011
    Citation: MAO Jinglin, LIU Kexing, HE Huizhong, GUO Xiaoxue, LIAO Zongwen. Effects of the activator on potassium release from potassium-rich shale and potassium feldspar and its mechanism[J]. Journal of South China Agricultural University, 2015, 36(1): 60-64. DOI: 10.7671/j.issn.1001-411X.2015.01.011

    活化剂对富钾页岩、钾长石的活化效果及作用机理

    Effects of the activator on potassium release from potassium-rich shale and potassium feldspar and its mechanism

    • 摘要:
      目的 综合利用我国丰富的非水溶性钾矿,以缓解我国钾肥市场“供-需”矛盾.
      方法 通过水浸提和盆栽试验,比较了活化剂QN对富钾页岩和钾长石的活化效果,并通过X衍射分析活化剂QN对富钾页岩和钾长石的作用机理.
      结果和结论 水浸提试验结果表明,在QN比例0.1%~10.0%范围内,富钾页岩、钾长石的活化效果不同,随QN比例的增加,活化页岩的水溶性钾释放量先增加后下降,1.0%QN活化页岩的水溶性钾累积量最高;活化钾长石的水溶性钾含量则随QN比例的增加而增加,QN比例为10.0%时的水溶性钾累积量最高.盆栽结果表明,活化页岩的玉米生物量显著高于富钾页岩,而与氯化钾的生物量相当;活化钾长石处理的玉米生物量与钾长石处理差异不显著,且显著低于氯化钾活化页岩处理.X衍射结果分析表明,QN活化富钾页岩和钾长石的作用机理是Na+与K+间的交换反应,活化页岩中新增的钠盐有K0.96Na0.04AlSi3O8、Na4Al2Si6O17·2H2O和Na6PbO4,活化钾长石中新增的钠盐为Na3Mn(PO4)(CO3).

       

      Abstract:
      Objective Comprehensive utilization of water-insoluble potassium resources is helpful to relieve the contradiction between supply and demand of potash market.
      Method The activated effects and fertilizer effects were studied by water extraction experiment and pot trial. The mechanism of activation was discussed by X-ray diffraction (XRD).
      Result and conclusion The results of water extraction experiment indicated that, within the QN ratio of 0.1%-10.0%, potassium-rich shale and potassium feldspar had different activated effects. With the increase of QN ratio, the water-soluble K extraction from potassium-rich shale increased and then decreased, and the activated ratio of 1.0% was the best. For potassium feldspar, the water-soluble K accumulative amount increased as the ratio of QN increased, and when the QN ratio was 10.0%, the accumulation of water-soluble K was the highest. The pot trail results showed that the pot biomass of activated K-shale was 49.42% higher than that of K-shale, reaching the potassium chloride level. For activated K-feldspar, the corn biomass was not significantly different from K-feldspar, which was lower than that of K-chloride and activated K-shale. The results of XRD analysis indicated that, the mechanism of QN activated potassium-rich shale and potassium feldspar was an ion exchange reaction between Na+ and K+. Some new sodium minerals can be found in activated K-shale and activated K-feldspar. In activated K-shale, the new sodium minerals include K0.96Na0.04AlSi3O8, Na4Al2Si6O17·2H2O and Na6PbO4, but it is Na3Mn(PO4)(CO3) in activated K-feldspar.

       

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