首页> 外文会议>Impact of Zeolites and Other Porous Materials on the New Technologies at the Beginning of the New Millennium >Zeolitized tuffs as pedogenic substrate for soil re-building. Early evolution of zeolite/organic matter proto-horizons
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Zeolitized tuffs as pedogenic substrate for soil re-building. Early evolution of zeolite/organic matter proto-horizons

机译:沸石凝灰岩作为土壤重建的生土基质。沸石/有机物原型地平线的早期演变

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An investigation was undertaken aiming to evaluate the suitability of zeolitized tuffs as an anthropogeomorphic material for soil re-building in degraded and desertified areas. Four artificial soil proto-horizons were prepared utilizing fine limestone gravel or Neapolitan yellow tuff as inorganic components, and sewage sludge or pellet manure as organic parent materials. The proto-horizons evolution was followed by analyzing leachates periodically collected over 80 days. After 80 days, the body of proto-horizons was also analyzed. Our results showed that the release of C- and N-compounds in the leachates was strictly dependent on the nature of the parent organic material. The presence of Neapolitan yellow tuff in the proto-horizon bodies clearly favored an advantageous evolution and stabilization of parent organic matrices, in optimizing the carbon to nitrogen ratios by increasing the C/N values, and by protecting the organic matter against a disproportionate degradation. Our findings led to conclude that the zeolitized tuff is a promising material in pedotechnique strategies for soil reconstruction and fight against desertification; on the contrary, the organic matter appeared to be excessively demolished in the presence of limestone gravel.
机译:进行了一项旨在评估沸石凝灰岩作为拟人化材料在退化和荒漠化地区重建土壤的适宜性的调查。以细石灰石碎石或那不勒斯黄凝灰岩为无机成分,污水污泥或颗粒肥料为有机母体,制备了四种人工土壤原型。在原始地平线演变之后,分析了在80天内定期收集的渗滤液。 80天后,还对原始地平线的身体进行了分析。我们的结果表明,渗滤液中C和N化合物的释放严格取决于母体有机材料的性质。在原始水平体中那不勒斯黄色凝灰岩的存在显然有利于母体有机基质的有利进化和稳定化,通过提高C / N值优化碳氮比,以及通过保护有机物不成比例的降解来促进其发展。我们的发现得出结论,沸石凝灰岩在土壤重建和防治荒漠化的土壤学技术战略中是一种很有前途的材料。相反,在石灰石砾石的存在下,有机物似乎被过度破坏。

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