Ippolito J A, Barbarick K A
Department of Soil and Crop Sciences, Colorado State University, Fort Collins, CO 80523-1170, USA.
J Environ Qual. 2006 Oct 27;35(6):2333-41. doi: 10.2134/jeq2006.0076. Print 2006 Nov-Dec.
In December 2003, the USEPA released an amended list of 15 "candidate pollutants for exposure and hazard screening" with regard to biosolids land application, including Ba. Therefore, we decided to monitor soil Ba concentrations from a dryland wheat (Triticum aestivum L.)-fallow agroecosystem experiment. This experiment received 10 biennial biosolids applications (1982-2003) at rates from 0 to 26.8 dry Mg ha(-1) per application year. The study was conducted on a Platner loam (Aridic Paleustoll), approximately 30 km east of Brighton, CO. Total soil Ba, as measured by 4 M HNO(3), increased with increasing biosolids application rate. In the soil-extraction data from 1988 to 2003, however, we observed significant (P < 0.10) linear or exponential declines in ammonium bicarbonate-diethylenetriaminepentaacetic acid (AB-DTPA) extractable Ba concentrations as a function of increasing biosolids application rates. This was observed in 6 of 7 and 3 of 7 yr for the 0- to 20- and 20- to 60-cm soil depths, respectively. Results suggest that while total soil Ba increased as a result of biosolids application with time, the mineral form of Ba was present in forms not extractable with AB-DTPA. Scanning electron microscopy using energy dispersive spectroscopy verified soil Ba-S compounds in the soil surface, probably BaSO(4). Wet chemistry sequential extraction suggested BaCO(3) precipitation was increasing in the soil subsurface. Our research showed that biosolids application may increase total soil Ba, but soil Ba precipitates are insoluble and should not be an environmental concern in similar soils under similar climatic and management conditions.
2003年12月,美国环境保护局发布了一份修订后的清单,列出了15种与生物固体土地施用有关的“暴露和危害筛选候选污染物”,其中包括钡。因此,我们决定监测旱地小麦(Triticum aestivum L.)-休闲农业生态系统实验中的土壤钡浓度。该实验在1982年至2003年期间每两年进行一次生物固体施用,每年施用量从0至26.8干公吨/公顷。研究在科罗拉多州布莱顿以东约30公里处的普拉特纳壤土(干旱古土壤)上进行。用4 M硝酸测定的土壤总钡含量随生物固体施用量的增加而增加。然而,在1988年至2003年的土壤提取数据中,我们观察到,随着生物固体施用量的增加,碳酸氢铵-二乙烯三胺五乙酸(AB-DTPA)可提取钡浓度呈显著(P < 0.10)线性或指数下降。在0至20厘米和20至60厘米土壤深度中,分别有7年中的6年和7年中的3年观察到这种情况。结果表明,虽然随着时间推移生物固体施用导致土壤总钡增加,但钡的矿物形态以AB-DTPA不可提取的形式存在。使用能量色散光谱的扫描电子显微镜证实了土壤表面存在钡-硫化合物,可能是硫酸钡。湿化学连续提取表明土壤亚表层碳酸钡沉淀在增加。我们的研究表明,生物固体施用可能会增加土壤总钡含量,但土壤钡沉淀物不溶,在类似气候和管理条件下的类似土壤中不应成为环境问题。