Dynamics of growth and seed production in the Siberian stone pine: The level and pattern of variation in characters

A statistical analysis of interannual variation in a set of vegetative and generative characters over 13 years has been performed to characterize the growth and seed production dynamics of the Siberian stone pine (Pinus sibirica Du Tour) in the southeast of the forest zone in western Siberia. The results have shown that the range of fluctuations in most of vegetative characters is ordinary and their distribution is close to normal. The range of fluctuations in many generative characters is enormous (from 0 to +∞), and the distribution of their values is usually skewed, with low values being recorded several times more frequently than high values. Most variable are the proportion of abortive cones and other characters that are determined mainly in the spring of the pollination year. These characters account for a very high level of variation in the total seed production.     

伊犁地区矿泉水资源及水化学特征

在介绍伊犁地区矿泉水资源与形成的水文地质条件的基础上，分析了矿泉水的化学组成及其特征，并给出了水化学类型。     

华南玄武岩红土化过程中微量元素地球化学

广东、海南的玄武岩．在强烈的红土化过程中．元素在红土剖面中发生迁移和残留、贫化和富集。根据红土化过程中元素的地球化学性状，将元素划分为活泼元素和不活泼元素两大类。并首次采用了元素它集因子这个概念来探讨红土化过程中微量元素的地球化学行为。最后讨论了红土化过程小金的表生富集作用。     

硫酸厂淤泥中SRB的选育及特性研究

从硫酸厂废水淤泥中分离筛选出了一株 SRB,其菌体形态呈弧状或细杆状 ,成熟细胞大小 0 .4～ 0 .6× 3 .0～ 5 .0μm,摇摆式运动 ,单极生鞭毛 ,芽孢染色阴性 ,革兰氏染色阴性 ;最适生长 p H6.0～ 6,5 ;适量氧气不会影响细菌生长 ,菌体内含过氧化氢酶。本文还探讨了该类细菌的分离培养方法 ,考察了分离菌部分生理生化特征及对硫酸盐还原能力 ,优化了培养基配方 ,并初步鉴定分离菌为脱硫弧菌     

Geochemical characteristics of rare earth elements in Wuhan section of the Yangtze River

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Recent developments of surface complexation models applied to environmental aquatic chemistry

1　ＢａｃｋｇｒｏｕｎｄＩｎｇｅｏｃｈｅｍｉｃａｌｃｉｒｃｕｌａｔｉｏｎ ,ｖａｒｉｏｕｓｐｏｌｌｕｔａｎｔｓｗｉｔｈａｄｖｅｒｓｅｉｍｐａｃｔｓ (ｅ .ｇ .,ｔｏｘｉｃｉｔｙ ,ｍｕｔａｇｅｎｉｃｉｔｙａｎｄｌｅｔｈａｌｉｔｙ)ａｒｅｕｓｕａｌｌｙａｓｓｏｃｉａｔｅｄｗｉｔｈｈｅｔｅｒｏｇｅｎｅｏｕｓｐａｒｔｉｃｌｅｓ,ｐｒｅｄｏｍｉｎａｎｔｌｙｃｌａｙｍｉｎｅｒａｌｓ .Ｇｅｎｅｒａｌｌｙ ,ｔｈｅｐｒｏｐｅｒｔｉｅｓｏｆｔｈｅｓｅｃｏｍｐｌｅｘｐａｒｔｉｃｌｅｓｓｈｏｕｌｄｂｅｄｅｓｃｒｉｂｅｄｕｓｉｎ…     

四川呷村多金属矿床地球化学特征及成因

呷村矿床是一个特大型的含金、稀土富银多金属矿床.成矿地质特征与日本黑矿相似.矿床形成于中低温、较低压的环境.成矿溶液为中等盐度、低密度水热体系.铅等成矿元素主要来自岛弧火山岩,硫和锶来自深部岩浆和海水,成矿水介质以大气降水为主,为典型海底火山热液—喷气沉积成因的块状硫化物矿床.     

岳山银铅锌矿床地球化学特征

本文通过对硫同位素、铅同位素、稀土元素、微量元素的研究，总结了安徽岳山银铅锌矿床的地球化学特征，并探讨了其成因，认为该矿床为火山一次火山气液作用形成的中低温热液型银铅锌矿床。     

四川彭州铜尾矿库植被特征分析与植物群落演替初探

本文分析了四川彭州铜矿尾矿库的植被特征、群落特征与演替。在该尾矿库上自然定居的高等植物共91种，隶属38科79属，以菊科（Compositae）和禾本科（Gramineae）植物为主。形成6种相对稳定的群落类型；在2003年弃耕后形成的地段分布有史蒿＋小飞蓬群落（Artemisia argyi＋Conyza conadensis Comm．）、艾蒿＋打破碗花花群落（Artemisia argyi＋Anemone hupehensis Comm．）、艾蒿群落（Artemisia argyi Comm．）和白车轴苹群落（Trifolium repens Comm．）；在经过30～40年自然演替的地段分布有芭茅＋羊耳菊群落（Miscanthus sinensis＋Inula cappa Comm．）和羊耳菊＋千里光＋密蒙花群落（Inula cappa＋Senecio scandens＋Buddleja officinalis Comm．）；在近十年内新形成的地段现主要覆盖地衣和葫芦藓（Funaria hygrometrica）。通过对群落结构和不同地段植被特征的对比，对本铜尾矿库的演替现状和规律进行了分析，井讨论了人为影响对演替进程的影响，提出了人工恢复措施的建议。     

HISTORICAL TRENDS IN SEDIMENTATION RATES AND SEDIMENT PROVENANCE,FAIRFIELD LAKE,WESTERN NORTH CAROLINA1

Sedimentation rates and sediment provenance were examined for lacustrine sediments deposited in Fairfield Lake, western North Carolina, during the past 111 years. Stratigraphic, radionuclide, and cartographic data indicate that sedimentation rates have increased several fold during the past three decades in response to localized development. The magnitude of increased sedimentation was surprising given limited development within the basin: 0.12 to 0.68 buildings/ha in 2000 in those parts directly delivering sediment to the dated cores. Thus, the analysis illustrates the potential sensitivity of watersheds in the southern Appalachians to changes in land cover. An approach that combined geochemical fingerprinting with sediment mixing models was subsequently evaluated to determine its ability to accurately estimate the contribution of sediment from (1) major bedrock formations that underlie the watershed and (2) potential sources associated with four land cover categories. Sediment sources in both analyses proved difficult to geochemically fingerprint to greater than 90 percent accuracy using data on acid‐soluble metals and selected isotopes of lead (Pb). The relative contributions of sediment from delineated sources, estimated by the mixing models, generally corresponded with known temporal and spatial patterns of land cover. However, the models were plagued by two significant problems — the chemical alteration of sediments as they were transported through upland streams to depositional sites within the lake and the loss of elemental mass. Thus, future investigations using the fingerprinting approach in this area of intense weathering, and presumably others, will need to modify the existing methods to more accurately elucidate changes in sediment provenance related to development.