Dipartimento di Fisica e Scienze della Terra, Università di Ferrara, Via Saragat 1, 44100, Ferrara, Italy.
Environ Monit Assess. 2014 May;186(5):2925-40. doi: 10.1007/s10661-013-3590-8. Epub 2013 Dec 29.
This geochemical study is focused on the easternmost part of the Po River alluvial plain in Northern Italy, which is interested by widespread agricultural activities, investigating a reclaimed sector of the Province of Ferrara, known as "Valle del Mezzano" (Mezzano Low Land, hereafter reported as MLL) characterized by peat-rich soils. The chemical-mineralogical characterization of these reclaimed soils is important to compare the local geochemical backgrounds with those recorded in other sectors of the River Po plain and to monitor if the observed concentration exceeds critical thresholds. The reported analyses include (a) measurement of the soil salinity, (b) nutrient evaluation, (c) major and trace element concentrations carried out on bulk soils, (d) tests of metal extraction with both aqua regia and EDTA to highlight the distinct elemental mobility and (e) phyto-toxicological measurement of heavy metal concentrations in plants (Lactuca sativa acephala) grown on the studied soils. The results indicate (1) high soil salinity, often with drastic increase of sodium and chloride along the soil profiles, (2) high nitrogen content (in part related to anthropogenic activities) on superficial horizons and nitrate decrease along the soil profiles and (3) comparative enrichments in heavy metals with respect to other soils of the province, which indicate that peat deposits are effective in trapping metals from anthropogenic sources. This, in turn, implies potential geochemical risks for the agricultural activities. In this regard, specific concerns are related to the high nickel and arsenic content of MLL soils due to the mobility of these elements and their attitude to be taken up by plants.
本地球化学研究集中于意大利北部波河冲积平原的最东端,该地区广泛开展农业活动,研究了费拉拉省(Province of Ferrara)一个已开垦的区域,称为“Mezzano 低地(Valle del Mezzano,以下简称 MLL)”,该区域以富含有机质的土壤为特征。这些开垦土壤的化学矿物学特征对于将当地地球化学背景与波河平原其他地区记录的背景进行比较以及监测观察到的浓度是否超过临界阈值非常重要。报告的分析包括:(a)测量土壤盐分;(b)养分评估;(c)对原状土进行常量和微量元素浓度分析;(d)使用王水和 EDTA 进行金属提取测试,以突出不同的元素迁移性;(e)在研究土壤上生长的植物(生菜)中进行重金属浓度的植物毒性测量。结果表明:(1)土壤盐分高,沿土壤剖面常伴有钠和氯的急剧增加;(2)表层土壤中氮含量高(部分与人为活动有关),而硝酸盐沿土壤剖面减少;(3)与该省其他土壤相比,重金属含量富集程度较高,这表明泥炭沉积物可有效捕获人为来源的金属。反过来,这意味着农业活动存在潜在的地球化学风险。在这方面,由于这些元素的迁移性以及它们被植物吸收的倾向,MLL 土壤中的镍和砷含量较高,这引起了特别关注。