800 MPa级双相组织低屈强比钢厚板研究

对基本成分为Fe-0.1C-Mo的微合金HSLA钢进行了变化轧制与冷却参数的试验,分析了钢的组织形貌及微观结构;研究了变形和冷却参数与钢的屈强比、缺口冲击功、延伸率等的关系.结果表明:通过对轧制、冷却工艺的组合与变化,实现对钢的强度、塑性、屈强比的控制;抗拉强度800 MPa级的厚钢板,其屈强比控制在0.75以下,低温冲击韧性良好.钢的组织主要由针状铁素体和马氏体两相组成.     

Functional characterization of cadmium-responsive garlic gene AsMT2b： A new member of metallothionein family

METALLOTHIONEINS(MT)ARE LOW-MOLECULAR-WEIGHT AND CYSTEINE-RICH PROTEINS.THE FIRST MT PROTEIN WAS ISOLATED FROM EQUINE RENAL CORTEX IN1957[1].GENES EN-CODING MTS OCCUR IN DIVERSE ORGANISMS SUCH AS ANIMALS,HIGHER PLANTS,EUKARYOTIC MICROORGANISMS AND IN SOME…     

不同水质灌溉对作物中重金属积累和分布影响的研究

对邯郸市5种水质灌区作物中的重金属进行了含量测定,分析了不同水质灌溉对小麦和玉米体内重金属积累和分布的影响。     

3种金属离子对球等鞭金藻生长的影响

利用分批培养,采用f/2培养基,研究了不同浓度的重金属离子(Cu2 、Pb2 、Cd2 )对球等鞭金藻生长的影响.结果表明,等鞭金藻的生长属于"S"型曲线;Cu2 抑制球形等鞭金藻的生长;浓度低于3 mg/L的Cd2 促进金藻生长,高于3 mg/L时抑制其生长;Pb2 能够促进等鞭金藻的生长.     

一次江淮大暴雨嵌套数值模拟试验

利用MM5非静力平衡模式，设计了未嵌套、两生和三重嵌套模式方案，对1999年6月23日一次江淮大暴雨过程进行了实际资料的降水个例试验，重点讨论了嵌套对数值模拟结果的影响。结果表明：嵌套后，随着水平分辩率的提高，模拟的降水量越来越大；三重嵌套的中间层细网格已经可以把雨区范围、降水中心位置、降水强度比较接近实况地模拟出来，最内层累网格中模拟出若干个β中等尺度降水中心；嵌套后内层细网格信息的外传会使外层粗网格的模拟结果有所改善。     

考洲洋表层沉积物的重金属含量及其污染分析

用原子吸收光谱法测定了南海东北部考洲洋表层沉积物中重金属的含量，各测站镉和铅含量超标率分别达到91.7%和50%，铜、锌含量未见超标，镍含量较低，比较和回归分析表明，考洲洋表层沉积物重金属含量在广东沿海居中等水平，并表现出同源相关关系，元素相关图显示，考洲洋表层沉积物尚未受人为来源镉和铅的影响。     

赋权图中最重的最长v-路与赋权周长

对2－连通非Hamilton赋权图G,本文证明：若P（u,v)是G中最重的最长路，则G的赋权周长C^w(G)≥d^w(u) d^w(v)，假设G满足文中描述的额外条件C1，C2，则max｛d^w(x),d^w(y)|d(x,y)=2｝≥m/2时，对每个顶点v,G含量最重长v-路P（u,v)使d^w(u)≥m/2，而d^w(x) d^w(y) d^w(z)≥m（当d(x,y,z)=2)时，c^w(G)≥2m/3.改进了非赋权图的周长及赋权图的赋权周长的若干已有结果。     

廉州湾重矿物组合区与泥沙来源

对廉州湾50个沉重物样品0.125-0.063mm粒级的重矿物（比重大于2．89的碎屑矿物）分析，发现3个重矿物组合区：（1）南流江口物区即电气石－锆石－钛铁矿－浅渌角闪石组合区；（2）西南部大风江口矿物区即钛铁矿－电气石－锆石组合区；（3）东南部北海港矿物区即电气石－钛铁矿－锆石－黑云母组合区。陆相径流（南流江流域）来沙是廉州湾的主要物源，也有部分物源是来自南部海岸的侵蚀物质，海相来沙是很少的，海湾泥沙运移总趋势是自东北向南运移，但南部沿岸泥沙自西南向东北运移。     

有机硅固砂剂在河南油田的开发与应用

为了克服河南油田地层胶结疏松及经过钻井、采油等作业过程对地层的激励作用而引起的地层出砂 ,开发研究了有机硅高温固砂剂 ,并在河南油田井楼、古城两个稠油油田 1 0口井进行了现场应用 .结果表明 :该剂在 2 0 0℃以上固化的岩心可耐 35 0℃以上的高温 ,抗折强度大于 3.0 MPa,抗压强度大于 8.9MPa,单井有效期平均长达 3个月 .现场使用结果证明该固砂剂效果良好 ,可以推广使用     

Bioaccumulation processes in ecosystems

The fate of environmental pollutants — the various isotopes of elements, and inorganic or organic compounds — is a fundamental aspect of ecology and ecotoxicology, and bioaccumulation is a phenomenon often discussed in this context. Human activities have drastically altered natural concentrations of many substances in the environment and added numerous new chemicals. An understanding of the processes of bioaccumulation is important for several reasons. 1) Bioaccumulation in organisms may enhance the persistence of industrial chemicals in the ecosystem as a whole, since they can be fixed in the tissues of organisms. 2) Stored chemicals are not exposed to direct physical, chemical, or biochemical degradation. 3) Stored chemicals can directly affect an individual's health. 4) Predators of those organisms that have bioaccumulated harmful substances may be endangered by food chain effects. While former theories on the processes of bioaccumulation focused on single aspects that affect the extent of accumulation (such as the trophic level within the food chain or the lipophilicity of the chemical), modern theories are based on compartmental kinetics and the integration of various environmental interactions. Concepts include results from quantitative structure-activity relationships (QSAR), pharmacokinetics, ecophysiology and general biology, molecular genetic aspects and selection, and finally the structure of communities and man-made alterations in them.