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Trace metal enrichment in sugarcane soils due to the long-term application of fertilisers, North Queensland, Australia: geochemical and Pb, Sr, and U isotopic compositions

机译:由于长期施用化肥,澳大利亚北昆士兰州对甘蔗土壤中的痕量金属富集:地球化学和铅,锶和铀同位素组成

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摘要

This study aimed to determine whether >80 years of fertiliser application has led to recognisable changes in the trace metal (Cd, Cu, Mo, Ni, Pb, Sr, Th, U, Zn) chemistry of topsoils (0–0.10 m) from sugarcane land, northern Queensland, Australia. The metal concentrations of commercial nitrogen (N) and potassium (K) fertilisers currently used in northern Queensland were generally lower than those of phosphate fertilisers and fertiliser blends. Composite topsoil samples (0–0.10 m depth) taken from canelands had higher median Cd, Mo, Pb, Sr, Th, U, and Zn concentrations than topsoils from forested areas of the catchment. Niobium, Ta, and Ti were confirmed as refractory immobile elements and used as reference elements for the evaluation of trace metal enrichments. Bivariate plots of trace metal/immobile element ratios verified that Cd, Mo, Pb, Sr, Th, U, and Zn are enriched in sugarcane soils compared with background forest soils. Isotopic ratios for Pb, Sr, and U highlight that fertilisers, cane soils, and forest soils have isotopically distinct compositions. Phosphate fertilisers currently used in the agricultural industry possess the most radiogenic 87Sr/86Sr, 234U/238U, 207Pb/206Pb, and 208Pb/206Pb ratios. Background forest soils have the highest 87Sr/86Sr, 207Pb/206Pb, and 208Pb/206Pb and lowest 234U/238U ratios. By contrast, cane soils exhibit 207Pb/206Pb and 208Pb/206Pb ratios that appear on a mixing line between the isotopically distinct background soils and phosphate fertilisers. Also, cane soils possess 234U/238U ratios similar to phosphate fertilisers. Thus, the application of phosphate fertilisers to canelands has resulted in higher Cd, Mo, Pb, Sr, Th, U, and Zn concentrations and more radiogenic Pb, Sr, and U isotope ratios in cane soils. Trace metal ratios and the Pb, Sr, and U isotopic composition of topsoils and fertilisers are useful tools to recognise fertiliser-derived trace metals in agricultural landscapes.
机译:这项研究旨在确定施肥> 80年是否导致了表层土壤(0–0.10 m)中痕量金属(Cd,Cu,Mo,Ni,Pb,Sr,Th,U,Zn)化学成分的可识别变化澳大利亚昆士兰州北部的甘蔗地。当前在昆士兰州北部使用的商品化氮(N)和钾(K)肥料的金属浓度通常低于磷酸盐肥料和肥料混合物的金属浓度。取自甘蔗地的复合表层土样品(深度为0–0.10 m)比流域森林地区的表层土壤中的Cd,Mo,Pb,Sr,Th,U和Zn浓度更高。铌,钽和钛被确定为难熔的固定元素,并用作评估痕量金属富集的参考元素。痕量金属/固定元素比率的双变量图证明,与背景森林土壤相比,Cd,Mo,Pb,Sr,Th,U和Zn在甘蔗土壤中富集。铅,锶和铀的同位素比值表明,肥料,甘蔗土壤和森林土壤的同位素组成不同。当前用于农业的磷酸盐肥料具有最强放射源的87Sr / 86Sr,234U / 238U,207Pb / 206Pb和208Pb / 206Pb比率。背景森林土壤具有最高的87Sr / 86Sr,207Pb / 206Pb和208Pb / 206Pb,最低的234U / 238U比。相比之下,甘蔗土壤的207Pb / 206Pb和208Pb / 206Pb的比率出现在同位素不同的背景土壤与磷酸盐肥料之间的混合线上。同样,甘蔗土壤的比例与磷肥相似,为234U / 238U。因此,在甘蔗地上施用磷肥导致甘蔗土壤中的Cd,Mo,Pb,Sr,Th,U和Zn浓度更高,而放射性Bb,Sr和U同位素比更高。微量金属的比例以及表土和肥料的Pb,Sr和U同位素组成是识别农业景观中肥料衍生的微量金属的有用工具。

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    Lottermoser, Bernd G.;

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  • 年度 2009
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