中国典型湖泊沉积物中脂肪烃的分布特征及来源

以我国13个典型湖泊的表层沉积物为研究对象,对沉积物的w(TOC)和w(TN)的分布特征进行了报道.结果显示,西南、华南地区湖泊沉积物的w(TOC)和w(TN)要高于西北地区,华东地区湖泊沉积物最低.结合多个脂肪烃来源参数,初步探讨了13个典型湖泊表层沉积物中脂肪烃的分布特征及来源. 结果表明:湛江玛珥湖、四海龙湾、洱海、红枫湖和程海受脂肪烃污染严重,鄱阳湖和双塔水库受脂肪烃污染程度最轻;受水体高矿化度的影响,双塔水库沉积物中有机质的δ13C值明显偏正;湛江玛珥湖中来自自身固氮藻类的脂肪烃含量明显高,致使湛江玛珥湖沉积物的δ15N值明显低;由于四海龙湾特殊的地理环境,四海龙湾沉积物中来自陆源木本植物的w(C_27+C29)明显高.      

烟气脱硫喷淋塔气体旋流实验研究

提出在烟气脱硫喷淋塔烟气进口设置导流板或采用切向进口,使烟气在塔内螺旋流动,以延长停留时间,加强气液湍动接触,并可改善系统的负荷调节适应能力。对不同进口结构的塔内流速分布、压力损失进行了实验研究,得出了旋流强度、压力损失等随导流板角度的变化关系,并将旋流情况与常规的直流进行了比较。     

微磁场条件下pH冲击对微氧活性污泥表面性质的影响

研究了微磁场条件下pH冲击对处理低负荷葡萄糖废水的微氧活性污泥表面性质的影响。在pH=6.0和9.0的条件下对添加磁粉和无磁粉反应器微氧活性污泥进行15 d的冲击,而后调整pH=7.5进行5 d的恢复实验。对pH冲击下污泥絮凝能力FA、疏水性RH和表面电荷SC的变化情况进行考察,结果表明,有磁粉反应器的各项指标均优于无磁粉反应器。经过5 d的恢复实验,添加磁粉反应器污泥的各指标均能恢复到接近初始值,而无磁粉反应器污泥难以恢复到接近初始值。     

杭州西湖冬、春季水体光学特性比较

于2007年冬、春季对杭州西湖主要湖区的水下光合有效辐射进行了研究,主要从光学角度讨论西湖的水质状况及其影响因素. 选用美国LI-COR公司的水下光量子仪(LI-COR 192SA)分层测定光合有效辐射(PAR),同时测定透明度,叶绿素a,悬浮物(SS),总氮和总磷等理化因子. 通过对不同深度处水下辐照度进行指数回归得到光学衰减系数(K_d). 结果表明,西湖水质和水体光学条件冬季优于春季,ρ(叶绿素a)和ρ(SS)低,透明度和真光层深度高. 水下光合辐射的垂直分布呈指数衰减. 从总体上来看,K_d冬季小于春季,外西湖高于其他湖区,并且由南至北逐渐升高. 冬、春季K_d分别为0.49～2.25和0.59～3.45 m－1. K_d与ρ(叶绿素a)和ρ(SS)呈正相关.浮游植物和悬浮物是影响西湖水下光照的重要因素. 降低浮游植物和悬浮物含量是改善西湖水体光学条件的重要内容.      

中国红色粘土型金矿成矿特征

中国的红色粘土型金矿是 90年代初发现并开始研究的 ,基本上产于南方特别是西南地区。由于特殊的地质构造条件和气候、地貌条件 ,该类型金矿与国外的红土型金矿存在明显的差异 :红色粘土型金矿剖面发育差 ,红土化程度低 ;对源岩依存度高 ;铁铝含量低、硅含量高 ;矿石处在富粘土矿物阶段 ,少见三水铝石 ,一般为伊利石和高岭石共存。金在红色粘土中以微细粒分散形式存在 ,且在红色粘土剖面中由于表生淋滤作用而发生活化、迁移和再沉淀。     

不同甘蔗基因型光合特性的数值分类

对30个甘蔗基因型光合性状进行数值分类、主成分、聚类和判别分析研究认为，甘蔗基因型间光合性状存在较大差异；利用主成分分析选出3个主成分，方差累计贡献率达到98．5％，蒸腾速率、气孔导度为第一主成分的主导因子，而净光合速率和气孔导度分别为二、三主成分的主导因子；经系统聚类将30个基因型分为三大类，在聚类分析基础上用判别分析选出对甘蔗光合性状数值分类有显著影响的4个光合参数，建立3个判别能力较高的判别模型．表5图1参22     

Identification of Tsuga Germplasm by Morphological Characters and RAPD Markers

Germplasm collection is important to preserve and maximize genetic diversity for germplasm conservation. Tsuga dumosa （ D. Don） Eichler in Engler ＆ Prantl. and T. chinensis var. forrestii （Downie） Silba germplasm was collected from three localities in China： Mt. Yulong, Wenfeng Temple and Mt. Dishiergu, Yunnan Province. Accessions were identified based on morphological characters and RAPD markers. The shapes of the apices and margins of needles were examined, and the length and width of needles, cones and seeds from accessions of mature plants were used to compare the morphological differences and to identify the germplasm. Molecular markers generated by randomly amplified polymorphic DNA （RAPD） were also used to characterize the taxa. Although the clustering based on RAPD markers was inconsistent with the morphological characters of the needles, based on the overall morphological characters and on RAPD markers, the accessions from Mt. Yulong and Wenfeng Temple were identified as T. chinertsis var. forrestii, and those from Mt. Dishiergu identified as T. dumosa. Taxonomic identification of the accessions was made based on morphology and by RAPD markers concurred. The results indicate that the shapes of the apices and margins of needles particularly from young plants could not be used as a possible key to identify T. dumosa and T. chinertsis var. forrestii. Fig 6, Tab 3, Ref24     

风化铬渣与新鲜铬渣中六价铬溶出特性的研究

采用直接淋浸法对风化铬渣及新鲜铬渣进行了六谷铬溶出的条件试验，60min的浸泡时间，80目以下的粒度对渣水比250g/200mL的新渣中Cr(VI)浸出率达69．4％，渣水比250g/200mL,500g/400mL,750g/600mL的风化渣中Cr(VI)的总溶出率分别为70．2％，86．3％，94．0％，其中第一次淋滤溶出率分别达48．1％，70．0％，81．6％，低PH值的淋浸水有利于Cr(VI)的浸出，在PH值为3时溶出率达高峰，Cr（VI）浸出质量比自然条件（近中性）高出14．1％－16．3％，增大管径和降低装置的滤面负荷可提高浸出效果，在直径80mm管径，500g铬渣装填料，滤面负荷9．95g/cm^2时，Cr（VI）溶出率达98．7％，真空抽滤可提高Cr（VI）浸出速率，但降低了滤液中Cr（VI）的浓度和溶出质量，上述试验结果表明了直接淋浸法回收铬渣中六价铬的可行性，并可作为工业化装置的设计参数。     

长乐—南澳变质带显微构造和岩组特征及应力场分析

通过光学显微镜和高压电子显微镜对带内的变形石英进行显微构造超微构造观测和估算变形参数(σ_1-σ_3=85.0MPa,ε_s=10~(-9)～10~(-10)/S),认为该区变质岩形成于深层环境,是长期缓慢变形的结果。变形石英位错构造为变形阶段和恢复阶段的混合体,其变形机制为塑性形变。采用石英光轴干涉图法,在偏光显微镜下对水平定向薄片进行岩组测量,绘制成该区的石英光轴方位图,探讨其构造变形的演化历史。首次划分出S(或S+S)和B+S构造岩岩组类型及Ⅰ型、Ⅳ型和Ⅴ型石英定向类型。应力场随着构造变形的演化作逆时针旋转。山南北挤压应力场逐渐变为单向推挤的应力场,从而认为构造变形是多期次的叠加。     

Factor analysis and linear regression model (LRM) of metal speciation and physico-chemical characters of groundwater samples

An approach is described for viewing the interrelationship between different variables and also tracing the sources of pollution of groundwater of north Chennai (India). The data set of 43 variables which include major ions, minor ions and trace metal speciation (Cu, Pb, Cd and Zn) collected during the pre-monsoon and post-monsoon seasons of the year 2000–2001, was subjected to R-mode factor analysis to comprehend the distribution pattern of the said variables. It was found that first factor measures salinity and hardness which explained 19.12% of the total variance (comprised of variables EC, TDS, Na⁺, K⁺, Ca²⁺, Mg²⁺, total hardness, Cl⁻ and SO₄ ²⁻) during pre-monsoon, while it was 25.08% during post-monsoon. The second and third factors were attributed to speciation of zinc and copper ions during both pre-monsoon and post-monsoon. Although there were two more factors, loaded with speciation parameters of lead and cadmium, the variance of them were less than 10%. From this study it is seen that sea water intrusion, municipal solid waste disposal are the identified sources of component of pollution. The importance of metal ions is taking a secondary role and the anthropogenic origin-industrial activity, is the reason in the evaluation of pollution status as they come in the second, third, fourth and fifth factors. As the trace metal speciation was grouped in separate factors, linear regression model (LRM) with correlation analysis was applied to check its validity for prediction of speciation and to apply LRM for rapid monitoring of water pollution.