巴西废石灰石的化学矿物学特征和土壤反应性

Leyser Rodrigues Oliveira , Humberto P. Cunha , Nilvânia M. Silva , Ivani P.M. Pádua
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引用次数: 7

摘要

本文评价了在巴西米纳斯吉拉斯州开采的四种废石灰石及其作为土壤酸度改良剂的潜力及其对土壤肥力属性的影响。在Formiga大学中心(UNIFOR)进行了实验室和温室实验,并在当地条件下收集了Oxisols。采用随机试验设计,设4个重复,5种石灰化材料(4种废石灰石产品+ 1种混合纯产品进行比较)以两种石灰化率(50%和70%的碱性饱和度)施用,并设置一个对照区(不施用石灰)。采用原子吸收分光光度计和x射线衍射对各石灰材料的CaO(%)、MgO(%)和微量元素Ca、Mg、Fe、Cu、Mn、Zn含量进行了表征。结果表明,所有石灰材料均可作为钙、镁的补充源,导致土壤pH、钙、镁和碱饱和度升高,而铝饱和度降低。白云石、方解石和石英是主要矿物。在所有废石灰石中都发现了微量的铜、铁、锰和锌,这被认为是此类产品的典型特征。考虑到改善化学特性和增加土壤肥力,使用废石灰石是一种替代方案,允许在小型物业中使用商业废弃材料。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Chemical and Mineralogical Characterization and Soil Reactivity of Brazilian Waste Limestones

This paper evaluated four waste limestones mined in the Minas Gerais State, Brazil, and its potential as soil acidity amendments and its effects upon soil fertility attributes. Laboratory and greenhouse experiments were performed at the University Centre of Formiga (UNIFOR), with Oxisols collected under native conditions. A randomly experimental design was set with four replications, five liming materials (four waste limestones products + a mix pure product, to comparison) applied in two liming rates (50% and 70% of base saturation), and a control plot (no lime applied). Each liming material was characterized with respect to CaO(%), MgO(%), and micronutrients Ca, Mg, Fe, Cu, Mn, Zn contents by atomic absorption spectrophotometer and the mineralogy by X-ray diffractometry. Results indicated that all liming materials tested could be classified as supplemental source of calcium and magnesium and caused an increase in soil pH, soil Ca and Mg, and base saturation levels, whereas aluminum saturation decreased. Dolomite, calcite and quartz are major minerals. Cu, Fe, Mn, and Zn were found in trace-amounts in all waste limestones, which was considered typical for such products. Considering the improvement of chemical characteristics and increase soil fertility, the use of waste limestone is an alternative that allows the use of commercial discarded material in small properties.

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