Vegetation patterns and nature reserve construction in an extremely-arid desert in Anxi,NW China's Gansu Province

Anxi County is located in the northwestern part of the Hexi Corridor in gansu Province and has the sole national level nature reserve of extremely-arid desert in China.Phytosociological methods (Braun-Blanquet,1964) are used to classify plant community types in this area.Eleven are disting uished,including six of deserts,four of oases and one transitional type between deserts and oases.Direct gradient analysis (DCA) is employed to correlate the distribution of plant communities to physiogeographic conditions.This study makes clear that water is the most important ecological factor for the distribution of plant species and communities in this area.The effects of water have been demonstrated in different ways.A vegetation gradient from lower altitude to higher altitude in the southern part of the reserve is driven by a precipitation gradient.The effects of the depth of ground water table contribute to the differentiation of vegetation from desert to oasis in the flat area.In a finer scale,the washed gullies have obviously higher species richness and also higher vegetation cover than the surround gobi surfaces,possibly caused by the effects of floods.The vegetation patterns demonstrate that the area of Anxi County is a complete landscape unit.The range of the current nature reserve is not large enough for the purpose of conserving the unique biodiversity in this area.     

生物传感器快速测定BOD在海洋监测中的应用

选用一株耐高渗透压的酵母菌种作为敏感材料可以实现BOD的快速测定。采用海藻酸钙包埋法和聚乙烯醇包埋法两种细胞固定化方法并进行了比较。就聚乙烯醇固定化微生物进行了渗稼压和重金属离子影响的研究。     

Developing Canada's National Forest Carbon Monitoring, Accounting and Reporting System to Meet the Reporting Requirements of the Kyoto Protocol

The rate of carbon accumulation in the atmosphere can be reduced by decreasing emissions from the burning of fossil fuels and by increasing the net uptake (or reducing the net loss) of carbon in terrestrial (and aquatic) ecosystems. The Kyoto Protocol addresses both the release and uptake of carbon. Canada is developing a National Forest Carbon Monitoring, Accounting and Reporting System in support of its international obligations to report greenhouse gas sources and sinks. This system employs forest-inventory data, growth and yield information, and statistics on natural disturbances, management actions and land-use change to estimate forest carbon stocks, changes in carbon stocks, and emissions of non-CO₂ greenhouse gases. A key component of the system is the Carbon Budget Model of the Canadian Forest Sector (CBM-CFS). The model is undergoing extensive revisions to enable analyses at four spatial scales (national, provincial, forest management unit and stand) and in annual time steps. The model and the supporting databases can be used to assess carbon-stock changes between 1990 and the present, and to predict future carbon-stock changes based on scenarios of future disturbance rates and management actions.     

海洋环境中混凝土桥的钢筋防锈技术

混凝土内部的高碱性能使钢筋表面形成一层钝化膜，保护钢筋免受锈蚀。然而，混凝土对钢筋的保护作用及其有效时间决定于混凝土的保护层厚度、混凝土质量、接触氯盐(来自原材料和环境)状况等因素。本文对海洋环境中混凝土桥的钢筋锈蚀原因进行了分析，并提出了相应的技术对策。     

天然林保护与东北地区水患治理方略

从天然林水文功能出发，阐述了东北地区天然林削减及其与洪涝灾害的关系，提出了东北地区水患治理方略。同时建议建立防汛信息系统，提高暴雨和洪水预报准确率以及防洪保险灾后重建。     

输气场站工艺安全风险分析

针对输气场站HAZOP风险评估出的天然气泄漏风险进行工艺安全量化分析,通过天然气泄漏喷射火模拟,对天然气泄漏风险进行量化,为输气场站的安全管理提供有效的技术支持。通过量化,分析出对天然气泄漏喷射火造成后果大小的影响因素,提高了HAZOP风险分析的准确性和科学性,对输气场站的风险管理具有参考意义。     

典型北方高碱度微污染水体强化混凝的示范研究

以高碱度、受有机物污染的典型北方水体为例,探索适宜的强化混凝技术.在水质调查的基础上,提出适合水质特征的强化混凝目标.研究了高碱度水体强化混凝技术方法.研究表明,可以通过3条技术途径提高水体中有机物的去除效率.其一在混凝前优化pH,促进絮凝剂水解形成中聚体,AlCl3在pH 6左右,FeCl3在pH 5左右时,有机物去除率可以提高一倍左右;其二是强化沉淀软化;其三是絮凝剂优化.结合我国实际情况,通过对传统絮凝剂进行改性,研制出了适合我国北方水质特征的高效絮凝剂,能较传统絮凝剂将有机物去除率提高30%以上.     

几种海洋微藻对水中三丁基锡化合物的迁移和转化作用

实验表明，在半抑制效应浓度下纤弱角毛藻，扁藻，三角褐指藻对三丁基锡均有瞬时强吸附作用，其后，微藻对三丁基锡的吸收可单室生物积累模型描述，根据模型曲线拟合求出其总吸收饱和浓度和生物排出速常数，微藻对三丁基锡的生物富集因子高达１０＾４－１０＾５，主要取决于高比表面，高分配比和高摄取速率，７２ｈ纤弱角毛藻对三丁基锡的生物降解率在５％左右。     

基于GIS的海洋环境质量评价图编制

本文介绍了采用地理信息系统技术制作海洋环境质量评价图的基本内容，重点阐述了图件的表现形式、编制过程和具体的操作方法，为海洋环境质量评价图的制作提供了一种新的方法。     

1952-2016年长江经济带天然与人为氮输入时空演变

过量氮输入是水体氮污染的关键驱动因子，解析氮输入的结构和时空变化模式成为氮素环境管理的重要基础和难点.基于1952—2016年长江经济带各地区氮活动数据，分别构建了天然氮输入和人为氮输入模型，评估了氮输入负荷的时空变化特征.结果表明：①长江经济带氮输入负荷总体越过EKC曲线拐点进入由增长向下降的发展阶段，拐点出现在人均GDP为35777~36299元·人^-1时，发生时间为"十二五"时期，主要原因是化肥和食物输入下降；②氮输入负荷存在显著的时空差异，东部地区表现为倒U型，中部为S型，西部为J型，表明氮负荷存在从东向西的空间转移，西部地区成为氮输入负荷增长的热点地区，这与东部地区化肥施用量下降有关；③人为输入是长江经济带氮输入的主要来源，输入量及其占总输入的比例均呈现显著的增长趋势，空间上表现为从西到东部逐步递增的变化规律，与氮驱动力分布一致；④植被的多年平均固氮量为1771 kg·km^-2·a^-1，其中，非农作物的固氮速率为763 kg·km^-2·a^-1，植被固氮量的年际波动较小，天然输入对长江经济带总体氮输入影响较小.