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八氢-1,3,5,7-四硝基-1,3,5,7-四氮杂环辛烷在土壤中的吸附与降解

Sorption and degradation of octahydro-1,3,5,7-tetranitro-1,3,5,7-tetrazocine in soil.

作者信息

Monteil-Rivera Fanny, Groom Carl, Hawari Jalal

机构信息

Biotechnology Research Institute, National Research Council of Canada, 6100 Royalmount Avenue, Montréal, Quebec, Canada H4P 2R2.

出版信息

Environ Sci Technol. 2003 Sep 1;37(17):3878-84. doi: 10.1021/es030407e.

Abstract

The sorption/desorption and long-term fate of octahydro-1,3,5,7-tetranitro-1,3,5,7-tetrazocine (HMX) was examined using sterilized and nonsterilized soils. Two soils were used that differ mainly by the amount of total organic carbon (TOC): an agricultural topsoil (VT, 8.4% TOC) and a sandy soil (SSL, 0.33% TOC). The adsorption isotherms performed at room temperature were well-described by a linear model, which led to sorption distribution coefficients of 2.5 and 0.7 L kg(-1) for VT and SSL soils, respectively. The organic content of soil did not significantly affect HMX sorption. Over a period of 20 weeks, HMX degraded (60% disappearance) in static anaerobic nonsterile VT soil preparations. In separate experiments using UL-[14C]-HMX, 19% mineralization (liberated 14CO2) was obtained in 30 weeks. In addition, four nitroso derivatives of HMX were detected. Knowing the sorption/desorption behavior and the long-term fate of HMX in soil will help assess the effectiveness of natural attenuation for HMX removal.

摘要

使用经过灭菌和未灭菌的土壤研究了八氢-1,3,5,7-四硝基-1,3,5,7-四氮杂环辛烷(HMX)的吸附/解吸及长期归宿。使用了两种主要因总有机碳(TOC)含量不同的土壤:一种农业表层土(VT,TOC含量8.4%)和一种砂土(SSL,TOC含量0.33%)。在室温下进行的吸附等温线用线性模型能很好地描述,这使得VT和SSL土壤的吸附分配系数分别为2.5和0.7 L kg⁻¹。土壤的有机含量对HMX吸附没有显著影响。在20周的时间里,HMX在静态厌氧未灭菌的VT土壤制剂中降解(消失60%)。在使用UL-[¹⁴C]-HMX的单独实验中,30周内获得了19%的矿化率(释放出¹⁴CO₂)。此外,还检测到了HMX的四种亚硝基衍生物。了解HMX在土壤中的吸附/解吸行为及其长期归宿将有助于评估自然衰减去除HMX的有效性。

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