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Natural Enrichment of Trace Elements in Surface Horizons of Calcareous Soils (La Mancha, Spain)

机译:石灰性土壤表层中微量元素的自然富集(西班牙拉曼查)

摘要

The study of five soil profiles developed on carbonatic sediments of Tertiary Miocene origin has been carried out. The topography of the area was basically flat and the traditional uses of the soils are the cultivation of dry cereals and grapevine. The geochemical characterization of the aforementioned profiles involves a study of the contents of major and trace elements among other pedologic aspects (texture, pH, organic matter, etc.). The results of this study also indicate a superficial enrichment of trace elements due to the leaching of Ca and moderate biological and anthropic activity. We can consider strontium, Sr, as the trace element that characterizes these limy soils (435 mg/kg average content in total soil and 708 mg/kg in the original rock). These contents are similar to the average value in Castilla-La Mancha of 380 mg/kg and are higher than the average in world soils of about 200 mg/kg. High levels of dangerous or pollutant elements (Cd, Hg, Pb, Cu, Zn, or Ni) were not detected. The majority of trace element anomalies are related to calcareous material and the leaching of calcium carbonate (Ca), while the influence of the anthropogenic factor is secondary. Soil quality does not indicate toxicity although surficial enrichment suggests a weak threat from consuming crops
机译:已经对中新世第三纪碳质沉积物上发育的五种土壤剖面进行了研究。该地区的地形基本平坦,土壤的传统用途是种植谷物和葡萄。上述剖面的地球化学特征包括研究其他主要方面(质地,pH,有机物等)中主要和微量元素的含量。这项研究的结果还表明,由于钙的浸出以及中等的生物和人类活动,微量元素的表面富集。我们可以将锶Sr作为表征这些石灰质土壤的微量元素(总土壤中的平均含量为435 mg / kg,原始岩石中的平均含量为708 mg / kg)。这些含量与卡斯蒂利亚-拉曼恰(Castilla-La Mancha)的平均值380 mg / kg相似,并且高于世界土壤中的平均值200 mg / kg。未检测到高含量的危险或污染物元素(镉,汞,铅,铜,锌或镍)。大多数微量元素异常与钙质物质和碳酸钙(Ca)的浸出有关,而人为因素的影响则是次要的。尽管表面富集表明食用农作物的威胁微弱,但土壤质量并不表示毒性

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