土壤有机质含量测定方法的改进研究

通过研究改进了土壤有机质含量的测定方法。首先称取适量土壤置于长管消解系统中进行消解,然后采用全自动电位滴定仪进行滴定,直接获得土壤的有机质含量。使用该方法测定的土壤标准样品的有机质含量均在保证值以内,同时对实际样品进行精密度测试,得到相对标准偏差为1．03％。该方法降低了土壤有机质含量检测的实验成本,减少了环境污染,同时提高了实验数据的准确度与精密度,值得推广。     

磁性纳米铁对厌氧颗粒污泥特性及其微生物群落的影响

考察了磁性纳米铁(Fe3O4NPs)对厌氧颗粒污泥溶解性微生物产物(SMP)、疏松胞外聚合物(LB-EPS)、紧密胞外聚合物(TB-EPS)的影响,同时利用高通量测序技术对厌氧颗粒污泥内微生物群落结构的变化进行了分析.结果表明,在长期接触实验过程中,投加Fe3O4NPs的反应器对COD去除率为83.6%,与对照组相比降低了5.7%.对照组与实验组中厌氧颗粒污泥TB-EPS含量(以VSS计)分别为178.20 mg·g-1和138.24 mg·g-1,而SMP含量分别为34.88 mg·L-1和27.44 mg·L-1;同时投加Fe3O4NPs后,在LB-EPS三维荧光(EEM)光谱中,紫外光区类腐殖酸荧光峰消失,辅酶F420荧光峰强度有所降低.在长期接触实验后,甲烷杆菌属(Methanobacterium)所占比例从76.15%增至86.76%,而甲烷丝菌属(Methanothrix)所占比例从17.1%降至7.51%,Methanothrix对于Fe3O4NPs更为敏感;总细菌群落变化明显,其中变形菌门(Proteobacteria)所占比例从66.44%降至47.16%,放线菌门(Actinobacteria)所占比例从8.97%增至17.33%,拟杆菌门(Bacteroidetes)所占比例从8.07%增至17.74%,厚壁菌门和拟杆菌门比例的增加对有机物的厌氧水解过程发挥积极的作用.     

连云港近岸海域2011~2016年环境变化研究

依据2011年2月~2016年1月在连云港近岸海域进行的19个季节航次海洋环境综合调查结果,分析探讨了该海域主要海水要素的季节变化趋势和相关性,结合历史资料阐述和评价了海域的营养状态水平、环境质量现状及变化趋势,对存在的环境问题进行了分析.结果表明：研究海域水质状况总体良好;水质评价结果显示无机氮（DIN）是海域内最主要的环境污染因子,且DIN含量近年来有逐渐增加的趋势,年均值已经超过二类海水水质标准;此外其他环境污染因子是活性磷酸盐（DIP）、化学需氧量（COD）和油类.调查期间研究海域处于富营养化状态,潜在富营养化分析显示氮磷比值（N/P）有逐渐增加的趋势;绝大多数季节的有机污染状况为轻度污染状态.研究结论对科学、系统的认识和评估连云港近海生态环境现状及预测未来生态环境变化趋势具有重要的参考价值,对连云港近海海洋生态环境的可持续发展具有十分重要的科学意义和实际应用价值     

中国乡村发展面临的挑战与长期性管理策略

分析研究了当前我国乡村发展所面临的严峻的挑战性问题，如乡村非农化进程停滞，城乡差异扩大带来的问题等；尤其是乡村生态破坏和环境污染危及到农业生产环境的安全和城乡居民的生存基础的情况，指出21世纪中国乡村发展相当迫切而艰巨；在可持续发展思想的框架下，提出了长期性管理策略，即类型管理、目标管理、乡村制度性投入的管理模式，并考虑了实现乡村可持续发展的制度创新与保障问题；随后针对乡村发展管理，构想了实施对策：即，1）积极推进城市化，缩减乡村人口总量；2）开展农业行业标准的制定和修订工作；3）推进乡村产业的科技创新步伐；4）强化生态环境观念，实行空间开发管制、尤其是生态脆弱地区。此外还需强调环境教育机制和广泛的公众参与机制。     

电除尘器分布板孔形对气流分布影响的仿真研究

针对不同气流分布板孔形,采用欧拉-拉格朗日多相流模型,应用CFX软件对电除尘器内部流场进行数值模拟计算,获得气流分布板孔形对气流均匀性影响的关系规律。仿真结果表明,孔形为方形的气流分布板能获得较佳的气流分布均匀性。     

深孔预裂爆破对含坚硬顶板高瓦斯煤层的综合作用研究

为研究深孔预裂爆破技术在含坚硬顶板高瓦斯煤层开采中的应用,以顾桥矿1123(1)工作面坚硬顶板为研究对象,基于小挠度理论建立了坚硬顶板垮落力学模型,导出了初次来压步距计算式;综合考虑瓦斯抽采需要,对深孔预裂爆破孔进行了优化设计,并在工作面顶板中开展了现场试验研究。结果表明:在工作面推进至27.3m时出现垮落,爆破后钻孔瓦斯流量显著增加,部分提高至30倍以上,瓦斯抽采量提高了3.5倍,初采期间安全回采煤炭25万吨,实现了坚硬顶板控制和卸压增透双重作用。     

特长隧道风仓接力通风关键参数及其效果研究

通过长斜井进入正洞施工的特长隧道,往往面临独头通风距离过长、工作面风量不足等问题,造成污染物难以在规定时间排出洞外。以衢宁铁路鹫峰山隧道风仓接力施工通风为依托,采用数值模拟方法研究了风仓长度、隔板长度及风机布置方式对轴流风机通风效率的影响,分析了原压入式通风和风仓接力通风洞内CO运移特性。结果表明,风仓长度从10 m增至25 m时,轴流风机通风效率大幅提高,风仓长度大于25 m时,对轴流风机通风效率的影响不大。设置中隔板会影响空气在风仓内的分流并产生较多旋流,从而降低风机通风效率;轴流风机远离斜井端对称布置,风仓内部风流的引流速度和引流范围最大,风流运动路径最优,通风效率最高。由于压入式通风受限于斜井断面尺寸及现场布置方式,当通风距离超过3 000 m后,无法满足洞内作业环境规定的条件。在正洞与斜井交叉部位设置密封的风仓,形成接力通风,能大幅度延长通风距离,提高通风效率,改善洞内空气质量。     

陆上原油长输管道泄漏爆炸事故情景构建研究

以某陆上原油长输管道为例,设定了陆上原油长输管道泄漏爆炸事故情景背景信息及演化过程,从预防、准备、预警、响应、恢复等阶段,梳理分析了事故情景应对全过程的任务及职责主体;针对各项任务从计划预案、人员队伍、装备物资、培训演练、运行机制等方面开展了情景应对能力评估;并针对存在的差距和不足,从企业和政府2个层面提出了针对此类情景的应急能力提升对策建议。该研究可为相关政府及企业加强油气长输管道事故应急准备能力建设提供参考。     

Time course of pyrrolizidine alkaloid sequestration in <Emphasis Type="Italic">Longitarsus</Emphasis> flea beetles (Coleoptera,Chrysomelidae)

Summary. Several species of Longitarsus take up, metabolize and store pyrrolizidine alkaloids (PAs) from their host plants. In feeding experiments using radioactively labeled PAs of different types we examined the time course of the sequestration process in L. jacobaeae and L. aeruginosus. We found that adapted species efficiently store PAs for at least two weeks without major losses. During that time, there is virtually no change in the ratio of tertiary alkaloids to stored non-toxic N-oxides, regardless of chemical form fed to the beetles. This implies a transient N-oxidation process where the alkaloids are only temporarily accessible to the enzyme. A dissection experiment with L. aeruginosus six days after uptake of labeled PAs showed that the tertiary alkaloids are not found in the hemolymph but are stored in the elytra and other body compartments. This conforms with earlier experiments that localized the enzymes site of action in the hemolymph. Furthermore we show that different total alkaloid doses in the diet of L. jacobaeae and the potentially less adapted L. succineus do not affect the ratio of recovered N-oxides to tertiary molecules. Thus, the efficiency of the N-oxidizing enzyme is not dependent on the concentration of alkaloids offered.     

What is the lesson from the unprecedented event over antarctica in 2002

Varotsos (2002a,b), suggested that both the smaller-sized ozone hole over Antarctica and its splitting in two holes in September 2002 occurred due to an unprecedented major sudden stratospheric warming caused by very strong planetary waves propagated in the southern hemisphere. Subsequently, a NASA press release of December 6, 2002, also reported the prevalence of very strong planetary waves in Antarctica. The aim of this Letter is to further discuss the morphology of the Antarctic ozone hole, to detect the causes that allowed the Antarctic stratosphere to exhibit this exceptional warming and to examine what it denotes about its mechanisms. Concerning the morphology, among the principal findings is that the ozone hole split occurred not only in the stratosphere but extended in the lower altitudes (upper troposphere). As to the causes of the major sudden stratospheric warming of 2002, a comparison with the previous warmings in Antarctica since 1964 is made. The smaller-sized Antarctic ozone hole of 2002 is approximately equal to that of 1988 when a strong sudden stratospheric warming occurred. If only the destruction of ozone by chlorofluorocarbons resulted in the delayed sudden stratospheric warmings in Antarctica, then the early sudden stratospheric warmings of 1988 and 2002 would not have occurred, since chlorofluorocarbon loading of the stratosphere has remained relatively stable in recent years. Furthermore, it appears that the El Nino characteristics in 1988 and 2002 are not similar.