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为进一步探究尾矿坝溃决后特有泥石流运移规律,掌握坝体破坏前至溃坝结束全流程发展状态,依托广东省某案例尾矿库为研究对象,采用基于有限元与离散元耦合方法的GDEM-PDyna软件构建泥石流类流体下泄演化数值模型,开展尾矿坝溃决演化分析,动态模拟尾矿库溃决过程中泥砂运动规律及淹没范围,并与MIKE 21软件计算结果进行对比。研究结果表明:尾矿坝溃决后,泥石流类流体流速升高、持续时间较短且尾砂流量发展迅速,2种模拟方法对比结果表明溃坝后坝基位置下泄流量变化与下游敏感点溃坝淹没深度变化情况一致。研究结果可为实现尾矿库下游重点区域灾害评估提供量化支撑,可有效提高尾矿坝溃决后灾害影响评估的精准性。 相似文献
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为了研究氮添加对森林土壤有机碳氮组分稳定性的影响,选取我国亚热带典型常绿阔叶林(浙江桂天然林和罗浮栲天然林)和针叶林(杉木人工林),开展为期5年的野外模拟氮沉降试验,分别设置对照〔0 kg/(hm2·a),以NH4NO3中的N计,下同〕、低氮〔75 kg/(hm2·a)〕和高氮〔150 kg/(hm2·a)〕3个氮添加水平,用H2SO4分2步酸水解获得LPⅠ(活性有机库Ⅰ)、LPⅡ(活性有机库Ⅱ)和RP(惰性有机库),定量研究土壤活性和惰性有机碳氮组分以及微生物生物量碳氮对氮添加的响应. 结果表明:氮添加仅对w(LPⅡ-C)(LPⅡ-C为活性有机碳Ⅱ)有显著影响,而对其他活性和惰性有机碳氮组分的影响不显著,并且对不同林分的影响存在差异. 与对照处理相比,低氮处理下浙江桂天然林、罗浮栲天然林和杉木人工林土壤w(LPⅡ-C)的增幅分别为15.3%、29.8%、68.8%;高氮处理下杉木人工林土壤w(LPⅠ-C)(LPⅠ-C为活性有机碳Ⅰ)、w(LPⅠ-N)(LPⅠ-N为活性有机氮Ⅰ)和w(RP-C)(RP-C为惰性有机碳)的增幅分别为32.4%、78.6%、28.7%;氮添加使得土壤w(SMB-C)(土壤微生物生物量碳)的增幅为18.1%~202.5%、w(SMB-N)(土壤微生物生物量氮)的增幅为0%~103.6%;在氮添加处理下,除杉木人工林土壤SMB-N/LPⅠ-N〔w(SMB-N)/w(LPⅠ-N)〕是随着氮添加水平的增加而降低外,微生物对其他林分土壤活性有机氮的利用均表现为随着氮添加水平的增加而增加. 研究显示,氮添加对阔叶林和针叶林土壤活性和惰性有机碳氮组分的影响存在差异,但差异不显著,这与它们归还土壤的凋落物性质差异有关,并且凋落物的分解差异也可能是影响土壤不同碳氮组分变化的原因. 相似文献
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An inventory of N(2)O emissions from agriculture in China using precipitation-rectified emission factor and background emission 总被引:5,自引:0,他引:5
Fertilized agricultural soils are a major anthropogenic source of atmospheric N2O. A credible national inventory of agricultural N2O emission would benefit its global strength estimate. We compiled a worldwide database of N2O emissions from fertilized fields that were consecutively measured for more than or close to one year. Both nitrogen input (N) and precipitation (P) were found to be largely responsible for temporal and spatial variabilities in annual N2O fluxes (N2O–N). Thus, we established an empirical model (N2O–N = 1.49 P + 0.0186 P · N), in which both emission factor and background emission for N2O were rectified by precipitation. In this model, annual N2O emission consists of a background emission of 1.49 P and a fertilizer-induced emission of 0.0186 P · N. We used this model to develop a spatial inventory at the 10 × 10 km scale of direct N2O emissions from agriculture in China. N2O emissions from rice paddies were separately quantified using a cropping-specific emission factor. Annual fertilizer-induced N2O emissions amounted to 198.89 Gg N2O–N in 1997, consisting of 18.50 Gg N2O–N from rice paddies and 180.39 Gg N2O–N from fertilized uplands. Annual background emissions and total emissions of N2O from agriculture were estimated to be 92.78 Gg N2O–N and 291.67 Gg N2O–N, respectively. The annual direct N2O emission accounted for 0.92% of the applied N with an uncertainty of 29%. The highest N2O fluxes occurred in East China as compared with the least fluxes in West China. 相似文献
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气体扩散电极(GDE)气液固三相界面可高效产生H2O2,但对铁离子还原能力较弱。针对这一问题,本文构建了一种基于缓释铁源的电芬顿体系(SRIS-EF),通过引入柱状铁棒与GDE电极协同作用加强体系的氧化能力。该体系旨在改进Fe2+投加方式,通过电场与溶液酸碱度协同作用持续生成Fe2+,提高羟基自由基(·OH)的生成和利用率,加速污染物的降解与矿化。以100 mg·L−1环丙沙星(CIP)为目标物,通过定量分析体系内生成的主要活性氧化物质(ROS)表征其氧化能力,结果表明SRIS-EF能够持续生成更高浓度的·OH。对比了不同体系对CIP的矿化能力,发现SRIS-EF的TOC矿化率与常规EF相比提高了12.1%。此外,考察了SRIS-EF体系中柱状铁棒面积、初始pH、电流密度等因素对降解效能的影响,得出了SRIS-EF体系的最佳条件为:铁棒面积2.89 cm2,初始pH 3.00,电流密度30 mA·cm−2,在此条件下反应60 min即可被完全去除CIP,处理360 min后TOC去除率可达47.3%。还对体系中无机离子和小分子有机酸的生成情况进行了测定,检测出CIP内的N和F主要以NH4+、NO3−和F−形式释放,降解过程中生成了草酸、甲酸、富马酸和丙二酸等四种短链羧酸,其中甲酸浓度较高。研究证实了SRIS-EF体系在降解水中难降解有机污染物方面优异的氧化性能。 相似文献
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CompoundpollutionofCd,Pb,Cu,Zn,Asinplant-soilsystemanditsprevention¥WuYanyu;WangXin;LiYing(InstituteofAppliedEcology,ChineseA... 相似文献
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Study on the proposed environmental guidelines for Cd, Hg, Pb and As in soil of China 总被引:4,自引:2,他引:4
This paper deals with the soil-environmental standard. According to the current situation of researching on the soil-environmental quality guideline at home and abroad, and on the basis of the foundations and principles of enacting the soil-environmental standard, the soil environment quality guideline values of Hg, Cd, Pb and As were suggested. 相似文献
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Chlortetracycline (CTC) is one of the most important pharmaceuticals occurring in the environment. An increase of its application as feed supplement for livestock and poultry in the world leads to a substantial CTC contamination of manures, because most of the CTC is excreted to manure. The simulation experiment of aerobic composting was adopted to investigate CTC depletion in aged and spiked manure composting, and to address the extent of CTC depletion during composting. The results showed that the extractable CTC initial concentration was markedly different between the different manures, with 94.71mgkg(-1) in broiler manure and 879.6mgkg(-1) in hog manure. The concentration of extractable CTC decreased rapidly at the initial stage of composting, and subsequently declined slowly during aged and spiked manure composting. At the end of composting, more than 90% of CTC in the manure composting process (42 days) was depleted, except for hog manure composting with a removal of only 27%. The CTC half-lives were 11.0 days in broiler manure, 86.6 days in hog manure, 12.2 days in layer-hen manure (150.3mgkg(-1) CTC), 12.0 days in layer-hen manure (100.0mgkg(-1) CTC) and 4.39 days in layer-hen manure (53.10mgkg(-1) CTC), all according to the first order kinetics. The significance of experimental parameters in CTC depletion was assessed by the Pearson correlation approach. Microbial degradation of CTC was not effective from manure composting. CTC depletion was in good correlation with total organic carbon, total nitrogen, total phosphorus, C/N, N/P and total heavy metals. 相似文献