RUNOFF RESPONSE FROM TWO RECLAIMED WATERSHEDS1

ABSTRACT: Detailed studies of the surface hydrology of reclaimed surface-mined watersheds for both rainfall and snowmelt events are non-existent for central Alberta yet this information is crucial for design of runoff conveyance and storage structures. A study was initiated in 1992 with principal objectives of quantifying surface runoff for both summer rainfall and spring snowmelt events and identifying the dominant flow processes occurring in two reclaimed watersheds. Snowmelt accounted for 86 and 100% of annual watershed runoff in 1993 and 1994, respectively. The highest instantaneous peak flow was recorded during a summer rainfall event with a return period of greater than 50 years. Infiltration-excess overland flow was identified as the dominant flow process occurring within the Sandy Subsoil Watershed, whereas saturation overland flow was the principal runoff process occurring within the West Watershed.     

假单胞菌XD-1(Pseuomonas XD-1)的产表面活性剂性能研究

从含油废水中分离到1株表面活性剂产生菌,经鉴定为假单胞菌(Pseuomonassp.),命名为XD 1.对假单胞菌XD 1的产表面活性剂性能进行研究,实验结果表明,在正交优化的培养基中发酵培养时,菌XD 1可将培养液的表面张力从70 0mN·m-1降至30 2mN·m-1,其产表面活性剂方式为生长相关型;经提取分析,菌XD 1所产表面活性剂为脂肽类和糖脂类物质的混合物,脂肽类物质为主要成分;菌XD 1所产表面活性剂的CMC值为50mg·L-1,在pH=6 0时表面活性剂表现出最佳活性;菌XD 1所产表面活性剂主要积累在胞内特定的细胞器中,并在细胞壁上产生一层粘附的表面活性剂膜,膜厚140nm,在生长过程中,菌体会将细胞器和细胞壁上的表面活性剂释放到胞外.将培养72h的菌体浸入双蒸水中,6h后菌体能把积累在细胞器和细胞壁上的表面活性剂释放到水体中.     

贵州独山锑矿田地质地球化学特征和构造动力热液成矿

独山锑矿田位于独山箱状背斜核部近倾伏端,矿床、矿体的产出严格受断裂控制,其半坡式锑矿呈脉状产于下泥盆统、志留系碎屑岩的陡倾斜断裂中;其巴年式的锑矿呈层状产于中泥盆统碎屑岩与碳酸盐岩之间的层间滑动带中。成矿温度低,矿石组分和围岩蚀变简单,锑主要来源于下伏地层,硫主要来源于赋矿地层．成矿流体主要为大气降水,构造动力成矿作用导致锑矿床的形成,矿床类型为一典型的构过动对热液矿床。     

厦门港表层水体中有机氯农药和多氯联苯的研究

利用ＧＣ－ＥＣＤ对厦门西港１９９８年７月取得上位表层水体中的１８种有机氯农药（ＨＣＨｓ，ＤＤＴｓ等）和１２种多氯联苯（ＰＣＢｓ）进行分析。其中有机氯农药的浓度范围６．６０～３２．６ｎｇ／Ｌ（其中ＨＣＨｓ：３．５１～２７．８ｎｇ／Ｌ），ｎｇ／Ｌ，ＤＤＴｓ，０．９５～２．２５ｎｇ／Ｌ均值１．４５ｎｇ／Ｌ），多氯联苯的浓度为０．０８～１．６９ｎｇ／Ｌ，同国内外其他港口海区相比较，其污染和蔼相对较低。同时     

从桂西北隆或金矿的地质地球化学特征看微细粒浸染型金矿的可能成因

在区域微细粒浸染型（卡林型）金矿床物源、成矿作用和构造控矿等方面研究的基础上，重点讨论了桂西北隆或金矿的地质地球化学特征。研究结果表明，该金矿店的穹隆构造、深断裂控矿、多层位赋矿和围岩蚀变等矿床地质特征，在滇黔桂三省区交界地区微细粒浸染型金矿中既具有普遍性，又表现出特殊性，其原生成矿硅质流体可能主要直接来自深部岩浆源分异作用，但由于是在地壳中成矿．不可避免地受到部分地层的物质和流体的混杂，因而属于地慢上隆－构造岩浆活化分异－深大断裂导矿－次级断裂、背科控矿－交代充填成矿的中偏低温热液金矿床。     

新疆赛都糜棱岩型金矿的矿石矿物学特征

本文首次详细论述了赛都糜棱岩型金矿的矿石类型、矿石组构和金属矿物的特征，对金矿物特征和金的赋存状态作了详细描述，并在矿石矿物学分析基础上提出了该金矿的矿化阶段。     

Speciation and fractionation of heavy metals in soil experimentally contaminated with Pb,Cd, Cu and Zn together and effects on soil negative surface charge

Speciation and fractionation of heavy metals in soil subsamples experimentally loaded with Pb, Cd, Cu and Zn in orthogonal design was investigated by sequential extraction, and operationally defined as water-soluble and exchangeable(SE), weakly specific adsorbed( WSA),Fe and Mn oxides-bound(OX) and organic-bound( ORG). The results showed that fractions of heavy metals in the soil subsamples depended on their speciation. About 90% of Cd and 75% of Zn existed in soil subsamples in the SE fraction. Lead and Cu existed in soil subsamples as SE, WSA and OX fractions simultaneously, although SE was still the major fraction. Organic-bound heavy metals were not clearly apparent in all the soil subsamples. The concentration of some heavy metal fractions in soil subsamples showed the good correlation with ionic impulsion of soil, especially for the SE fraction. Continuous saturation of soil subsamples with 0.20 mol/L NH4CI, which is the first step for determination of the negative surface charge of soil by the ion retention method, resulted in desorption of certain heavy metals from the soil. It was found that the percentage desorption of heavy metals from soil subsamples depended greatly on pH, the composition and original heavy metal content of the soil subsamples. However, most of the heavy metals in the soil subsamples were still be retained after multiple saturation. Compared with the parent soil, the negative surface charge of soil subsamples loaded with heavy metals did not show difference significantly from that of the parent one by statistical analysis. Heavy metals existed in the soil subsamples mainly as exchangeable and precipitated simultaneously.     

粤东一个类型独特的锡矿床

作者对西岭凤地山锡矿床的成矿地质条件,特别是火山构造、岩浆演化与成矿的关系进行了研究,认为:西岭锡矿是一个与火山侵出相碎斑熔岩时、空、成因关系密切的次火山热液脉状锡矿床。根据西岭锡矿的地质环境和成矿物理化学条件、矿质、水介质来源建立了理想的成矿模式。进而指出粤东斑岩锡矿的远景。西岭锡矿类型的确定,对粤东和赣南火山岩地区锡矿普查具有重要意义。     

示波极谱法测定地面水中的钒

应用钒（ Ｖ） ５ Ｂｒ Ｐ Ａ Ｄ Ａ Ｐ Ｈ２ Ｏ２ 体 系产生的 络合极 谱波对地 面水中 的钒 进行 了测 定，并 讨论了测试 条件。钒 浓度在 ００１ ～２２５ μｇ／２５ ｍ Ｌ 范围 内极谱 电流与钒 含量呈线 性关系 ，本法具有 较高的选择 性和灵 敏度，测定 地面水 中的钒结 果令人 满意     

三门火山盆地的层状矿床及其与盆地形成演化的关系

浙江三门中生代火山——沉积盆地的形成演化可分四个阶段。每一阶段均伴产有不同成因和各具特色的金属矿床,显示了陆相火山作用较为完整的成矿体系。其中层状矿床具有同生和后生的双重特征,多成因,多来源,是较典型的火山沉积——后期热液迭加改造型矿床。本文着重介绍它的主要特征及盆地的形成演化对火山成因矿床的控制。