首页> 外文期刊>Geoderma: An International Journal of Soil Science >Copper content of soils and river sediments in a winegrowing area, and its distribution among soil or sediment components.
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Copper content of soils and river sediments in a winegrowing area, and its distribution among soil or sediment components.

机译:酿酒区土壤和河流沉积物中的铜含量及其在土壤或沉积物成分中的分布。

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This paper concerns copper levels in the components of soils and river sediments in a river basin partially devoted to vineyards that are regularly treated with copper-bearing grapevine fungicides. Copper concentrations were determined in 26 soil samples, 20 river sediment samples and 71 river water samples taken in a small basin with steep slopes suffering significant erosion. Mean total Cu concentration was 31 mg kg-1 in woodland soils, 30 mg kg-1 in pasture soils, and eight times higher, 246 mg kg-1 (range 157-434 mg kg-1), in productive vineyard soils. Total copper concentration in river sediments ranged from 18 to 209 mg kg-1 depending on the proportion of land under vineyard in the sub-basin drained via the sampling point (r=0.915, p<0.05). Soils differed relatively little as regards the distribution of Cu among various fractions; in particular, about 50% of total copper content was generally bound to soil organic matter. The distribution of Cu in sediments was more heterogeneous: sandy sediments had copper distributions similar to those observed in soils, but in silty sediments with large inorganic colloids fractions it was these amorphous colloids that bound the largest proportion of copper (mean 31.5%). The absence of significant differences among water-soluble Cu concentrations at the various water-sampling points suggests that winegrowing does not increase water-soluble Cu levels in the river under normal circumstances.
机译:本文关注部分流向葡萄园的流域土壤和河流沉积物中铜的含量,这些葡萄园定期用含铜葡萄杀菌剂处理。在一个小坡度严重侵蚀的盆地中,测定了26个土壤样本,20个河流沉积物样本和71个河流水样本中的铜浓度。在林地土壤中,平均总铜浓度为31 mg kg-1,在牧场土壤中为30 mg kg-1,在生产性葡萄园土壤中,平均总Cu浓度为246 mg kg-1(范围157-434 mg kg-1),是后者的八倍。河流沉积物中的总铜浓度范围为18至209 mg kg-1,具体取决于通过采样点排放的子盆地葡萄园下的土地比例(r = 0.915,p <0.05)。就各部分之间的铜分布而言,土壤差异相对较小。特别是,总铜含量的约50%通常与土壤有机质结合。铜在沉积物中的分布更加不均匀:沙质沉积物的铜分布与在土壤中观察到的相似,但在具有较大无机胶体分数的粉质沉积物中,这些无定形胶体占铜的最大比例(平均31.5%)。在各个水采样点,水溶性铜浓度之间没有显着差异,这表明在正常情况下,葡萄种植不会增加河流中的水溶性铜含量。

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