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Pre- and Post-Mined Bauxite Soils of Jamaica: Physical and Chemical Properties

机译:牙买加开采前和开采后的铝土矿土壤:理化性质

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Earthy bauxite (aluminum ore) deposits over limestone bedrock cover over 20% of Jamaica's surface area. With the shortage of arable land in Jamaica, there is great interest in using post-mined bauxite lands for agriculture. The purpose of this study was to compare physical and chemical properties of pre- and post-mined bauxite soils that are relevant in assessing suitability of these lands for small-scale agriculture. Pedons were described and sampled for characterization at two pre-mined sites and four post-mined sites near Mandeville, Jamaica. Post-mined soils were generally steeper, shallower, and higher in limestone rock fragments than pre-mined soils. Pre-mined soils consisted of Ap and Bo horizons making up clayey Oxisols with low charge and low bulk density. The new caret (^) symbol, which indicates horizons formed from human transported material, was helpful in describing pedons of post-mined soils. Post-mined soils consisted of ^Ap horizons (replaced topsoil) and 2^C horizons (fill material) over limestone. Some post-mined pedons also had 2Bob or 3Bob horizons (Bo in situ buried by replaced topsoil and/or fill material). Post-mined soils had higher bulk density in the ^Ap horizons than pre-mined Ap horizons and higher pH throughout due to the incorporation of limestone rock fragments. In ^Ap horizons, organic matter and granular structure increased with time after reclamation and establishment of grass cover.
机译:土状铝土矿(铝矿石)沉积在石灰岩基岩 上,覆盖了牙买加20%以上的表面积。由于牙买加耕地的短缺,人们对利用矿山开采后的铝土矿土地进行农业生产产生了浓厚的兴趣。此 研究的目的是比较在评估 的适用性方面相关的pre- 和矿山铝土矿的物理和化学性质。小型农业土地。在牙买加曼德维尔附近的两个预采矿场和四个采后矿场,描述并取样了Pedons 进行表征。开采后的 土壤通常比开采前的土壤更陡峭,更浅,而石灰岩 岩石碎块中的土壤更高。预挖过的土壤由Ap和Bo层组成的 组成了低电荷 和低堆积密度的黏土质溶胶。新的插入符号(^)表示由人类运输的物质形成的 地平线,对描述开采后土壤的脚印很有帮助。采后土壤由石灰岩上的^ Ap层(替代表土)和2 ^ C层(填充材料) 组成。一些开采后的脚架也具有2Bob或3Bob 地平线(被替换的表土和/或填充 材料现场埋藏的Bo)。由于掺入了石灰石碎屑,后采土在^ Ap 地平线中的堆积密度高于采前Ap层,并且整个 的pH较高。在^ Ap 地平线中,开垦和建立草皮后,有机物和颗粒结构随 时间的增加而增加。

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