金沙江水系鱼体中稀土元素环境背景值研究

采用等离子发射光谱法测定了金沙江水系鱼体肌肉中十个稀土元素的含量。根据统计方法提供了金沙江水系鱼体中稀土元素环境背景值。它们分别是:La 0.064mg·kg~(-1),Ce 0.156mg·kg~(-1),Pr 0.080mg·kg~(-1),Nd 0.025mg·kg~(-1),Eu 0.002mg·kg~(-1),Dy 0.009mg·kg~(-1),Er 0.019mg·kg~(-1),Yb 0.007mg·kg~(-1)和Y 0.015mg·kg~(-1)。结果表明:金沙江水系鱼体肌肉中稀土元素含量与江水中溶解态稀土元素含量有关。同时获得了该水系十个稀土元素的生物富因子。     

赣江流域水文地理特征及影响经济发展的研究

本文以自然和经济条件为基础,分析研究了赣江流域降水、径流、泥沙、水质等水文地理特征,提出了开发利用赣江水资源、促进流域经济发展的主要措施.     

陕西黄河滩地农田鼠类调查

报道了1988年6—11月、1991年3—5月对陕西东部黄河滩地农田害鼠的种类、数量及分布调查的结果。计有鼠类9种,隶属3科。其中子午沙鼠、小家鼠、大仓鼠和黑线姬鼠为本地区的优势种。     

珠江三角洲文化形态论纲

珠江三角洲文化形态的性质是务实求利;其特征是商业俗文化;其结构由岭南文化、中原文化、港澳文化和西方文化四因素构成;其地位是有中国特色的社会主义新文化的“曙光”,是中华民族大一统文化的“中介”。     

攀西裂谷中段摩挲营花岗岩的流动构造初析

本文通过对摩挲营花岗岩体的流动构造研究,查明了岩浆侵位时流动空间的形态。岩浆是以十多度的倾角沿安宁河断裂由北向南流动冷凝的。在岩体中,流动构造由定向排列的斑晶和包体显示出来。斑晶是石岩浆结晶的中晚期形成的,主要是由于受到岩浆流体内部的应力作用而定向;包体是岩浆中的固体岩块,它必然受到流体的改造和冲击,其形态特点能反映岩浆的流动特征。这对弄清地球深郜的动力学特点,查明岩浆的侵位机制及指导寻找与岩浆作用有关的矿床都有重大意义。     

黄河沉积物中重金属离子的形态转化及释放研究

以黄河包头段上游清洁河段的沉积物为吸附剂,以Pb^2 、Cu^2 、Zn^2 、Cd^2 等多离子溶液为吸附质,开展了重金属离子被黄河沉积物吸附后的再释放,以及吸附作用对重金属形态转化的影响等实验研究．结果表明,重金属离子被黄河沉积物吸附后,各元素均不转入残渣态,Cu^2 和Zn^2 主要向碳酸盐结合态及铁锰氧化物结合态转化,Pb^2 主要向碳酸盐结合态和可交换态转化;Cd^2 主要转入可交换态和碳酸盐结合态．吸附后的赋存形态决定了Cd^2 的释放量及释放能力远远大于其它3种重金属离子,由Cd^2 排放引起的污染不易消除且影响长久．     

云南省金沙江流域生态环境建设的问题与对策研究--长江上游生态屏障建设重点地区调查报告之一

生态环境保护和建设是我国西部大开发的重要战略之一。云南省金沙江流域是长江上游生态脆弱地区,也是生态环境保护和建设的重点地区．在实地调研的基础上分析云南省金沙江流域地区的生态环境状况,探讨该区域生态环境建设中存在的主要问题,并提出了进一步加强该地区生态环境建设的对策建议．     

Regional patterns of particulate spectral absorption in the Pearl River estuary

Knowledge about the spectral absorption properties of marine particulate matters is of important signification for various goals of optical oceanography, among them the most concerns are the bio-optical algorithms for ocean color remote sensing[1], basic theory of light radiative transfer in water column[2], bio-optical models for estima-tion of primary productivity and simulation of the upper ocean ecological process[3,4]. The spectral absorption by marine particulate matter is combined influe…     

Change in the sedimentary environment of Wanquan River Estuary,Hainan Island,China

Pb geochronology and sediment core profiles of organic carbon, total sulfur and organic carbon isotope (d 13C) values were used to reconstruct the local environ-mental history of the Shamei Lagoon, located in the Wan-quan River Estuary, eastern Hainan Island, China. Totalsulfur and d 13C values decreased upwards in the top 30 cm of a sediment core that spanned the last 200 years of deposi-tion. Total sulfur concentration and d 13C values respectively decreased upward from 1.92% to 0.36%, and -20.63?to -23.64? The C/S ratio in the 19th century and earlier was relatively stable in the range of 0.47—0.80, and there was a positive correlation between organic carbon and total sulfur. Since around 1900 AD, the C/S ratio increased rapidly to a maximum of 3.94, but no simple correlation was found be-tween organic carbon and total sulfur during this more re-cent period. These results indicated that before 1800 AD, the lagoon had a fully marine character, and the location of to-day抯 Wanquan River Estuary was an open embayment.From 1800 to 1900, the salinity of Shamei Lagoon decreased noticeably. The amount of seawater which could enter thelagoon decreased gradually as the Yudai spit grew. Today,seawater scarcely affects the lagoon; it is essentially a fresh-water basin.     

Response of the accumulation of proline in the bodies of<Emphasis Type="Italic">Populus euphratica</Emphasis> to the change of groundwater level at the lower reaches of Tarim River

The content of proline in the plant bodies is closely related to the converse-succession-resistant capability of plants. Under the drought stress, the proline accumulates rapidly in the plant bodies for maintaining a certain mois-ture content and an expanding-pressure momentum in cells through the osmoregulation, thus the drought-resis- tant capability and the converse-succession-resistant ca-pability of plants are increased[1,2]. Many researches on the relationship between the proline and the…