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111.
S. Veerasingam R. Venkatachalapathy S. Sudhakar P. Raj V. Rajeswari 《环境科学学报(英文版)》2011,23(7):1129-1134
Eight mollusc species and sediment samples collected from three different stations along Tamilnadu coast, Bay of Bengal, India
were analysed for the levels of petroleum hydrocarbons to elucidate the status of the petroleum residues in mollusc meant for human
consumption. The concentrations of petroleum hydrocarbons in sediments along Tamilnadu coast varied from 5.04–25.5 g/g dw (dry
weight). High concentration of petroleum hydrocarbons in the sediment of Uppanar estuary (25.5 1.45 g/g dw) was perhaps land
and marine based anthropogenic sources of this region. The petroleum hydrocarbon residues in eight mollusc species collected from
Uppanar, Vellar and Coleroon estuaries varied between 2.44–6.04 g/g ww (wet weight). Although the concentration of petroleum
hydrocarbons in sediment of the Uppanar region was markedly higher than the background, the petroleum hydrocarbon residues in
mollusc collected from Uppanar estuary did not suggest bioaccumulation. The results signified that industrial growth has affected the
aquatic environments and regular monitoring will help to adopt stringent pollution control measures for better management of the
aquatic region. 相似文献
112.
人类正面临着严重的石油短缺,因此正在努力减少化石燃料的使用以抑制温室气体排放所造成的全球变暖趋势。在此紧要关头,风能、太阳能、生物燃料等可替代能源就显示出了重要性。由于目前西欧正逐渐成为世界上人口最稠密的地区之一,这使得西欧在推行替代能源的过程中面临 相似文献
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118.
Mengnjo J. Wirmvem Takeshi Oh Wilson Y. Fantong Samuel N. Ayonghe Jonathan N. Hogarh Justice Y. Suil Asobo Nkengmatia E. Asaah Seigo Ooki Gregory Tanyileke Joseph V. Hell 《环境科学学报(英文版)》2014,26(4):801-809
Rainwater characteristics can reveal emissions from various anthropogenic and natural sources into the atmosphere. The physico-chemical characteristics of 44 monthly rainfall events (collected between January and December 2012) from 4 weather stations (Bamenda, Ndop plain, Ndawara and Kumbo) in the Bamenda Highlands (BH) were investigated. The purpose was to determine the sources of chemical species, their seasonal inputs and suitability of the rainwater for drinking. The mean pH of 5 indicated the slightly acidic nature of the rainwater. Average total dissolved solids (TDS) were low (6.7 mg/L), characteristic of unpolluted atmospheric moisture/air. Major ion concentrations (mg/L) were low and in the order K+ 〉 Ca2+ 〉 Mg2~ 〉 Na+ for cations and NO3 〉〉 HCO3 〉 SO] 〉 CI- 〉 PO3- 〉 F- for anions. The average rainwater in the area was mixed Ca-Mg-SO4-CI water type. The CI-/Na+ ratio (1.04) was comparable to that of seawater (1.16), an indication that N a+ and CI originated mainly from marine (Atlantic Ocean) aerosols. High enrichments of Ca2+, Mg2+ and SO2- to Na+ ratios relative to seawater ratios (constituting 44% of the total ions) demonstrated their terrigenous origin, mainly from Saharan and Sahelian arid dusts. The K+/Na+ ratio (2.24), which was similar to tropical vegetation ash (2.38), and NO3 was essentially from biomass burning. Light (〈 100 mm) pre-monsoon and post-monsoon convective rains were enriched in major ions than the heavy (〉 100 mm) monsoon rains, indicating a high contribution of major ions during the low convective showers. Despite the acidic nature, the TDS and major ion concentrations classified the rainwater as potable based on the WHO guidelines. 相似文献
119.
建立了利用RP91C-RA915M汞分析仪直接测定土壤中总汞的方法。该方法直接固体进样,省去了常规方法加酸消解、赶酸、定容等繁琐的前处理步骤;利用标准土壤绘制工作曲线,无需反复稀释标准储备液配制标准溶液,测定了方法检出限、精密度及准确度。结果表明此方法准确、可靠,是一个比较理想的分析方法。本方法的检出限为0.25μg/kg,相对标准偏差为1.98%~4.92%,标准样品测定准确,加标回收率为92.8%~106%。 相似文献
120.
温带典型草原土壤总有机碳及溶解性有机碳对模拟氮沉降的响应 总被引:3,自引:1,他引:2
2008年5月~2011年10月,以内蒙古温带典型草原为研究对象,利用小区模拟控制试验,设置对照[0 g·(m2·a)-1]、低氮[5 g·(m2·a)-1]、中氮[10 g·(m2·a)-1]、高氮[20 g·(m2·a)-1]这4个净氮输入量处理,模拟研究了大气氮沉降水平变化对土壤总有机碳(TOC)以及溶解性有机碳(DOC)含量、年际变化及其垂直分布格局的影响,并分析了两者之间的关系.结果表明,除个别年份外,土壤TOC与DOC含量均随土壤深度增加而递减,4 a的连续施氮并未改变土壤TOC与DOC的垂直分布规律,但施氮降低了土壤TOC的垂直变异,增加了土壤DOC的垂直变异;施氮4 a对于草地表层0~20 cm土壤TOC与DOC含量的变化并未表现出显著影响(P>0.05).不同氮输入水平处理0~20 cm土层有机碳密度在3.9~5.6 kg·m-2之间变动,试验前两年不同氮处理0~20 cm土壤有机碳密度均低于对照或与对照接近,试验后两年,施氮对土壤总有机碳密度逐渐呈现出一定的促进作用,但与对照的差异仍不显著(P>0.05);不同处理0~20 cm土层DOC/TOC约为0.32%~1.09%,氮输入增加普遍降低了DOC在整个TOC中所占的比例;草地土壤TOC与DOC的变化呈显著正相关(P<0.01).不同处理草地土壤DOC随时间的变异均远大于TOC,与TOC相比,草地土壤DOC的变化更为迅速,是研究草地土壤碳库对氮沉降变化响应的重要敏感性指标. 相似文献