厦门西港和九龙江口浮游植物生化组成及其环境因子效应

厦门西港和九龙江口浮游植物碳水化合物与光强、盐度和叶绿素ａ均显著正相关，蛋白质与光强有负相关关系，脂类受光强的影响较小，蛋白质与碳水化合物之比与氮磷比显正相关。１０月该海域浮游植物叶绿素ａ与生化组分含量都比４月高，与１０月海水温度和海面辐照度较高有关     

基于DEM的山区旱灾风险评价模型——以西南地区为例

旱灾研究中,地形导致的水热再分配容易造成地域间旱灾灾情的明显差异,因此地形因子对于旱灾风险的准确评价及灾情的客观评估至关重要。采用气象站点观测数据和DEM数据,通过模拟复杂地形影响下的下垫面真实水分情况,加入地形因子的影响,建立了以干旱致灾因子(水分条件)、孕灾环境(地形)、承灾体(农作物脆弱性曲线)综合的旱灾风险评价三度模型;并以地形复杂、旱灾多发的西南地区为例,编制了旱灾风险等级图,以期为客观评估旱灾灾情,有效开展区域旱灾风险防范提供科学依据。     

The study on the dechlorination of OCDD with Pd/C catalyst in ethanol-water solution under mild conditions

Dechlorination of octachlorodibenzo-p-dioxin (OCDD) was carried out in ethanol-water (v/v=1:1) solution of NaOH in the presence of Pd/C catalysts with the use of H(2). The substrate was dechlorinated with Pd/C under mild conditions (atmospheric pressure and <100 degrees C) to give a chlorine-free product, dibenzo-p-dioxin (DD), in high yields. After reaction of 3h at 50 degrees C, 95.9% OCDD was degraded to low dechlorinated congeners and the yield of DD was 77.4%. We have also studied the dechlorination selectivity of chlorine atoms on the different substituted positions and postulated the dechlorination pathway of OCDD. For OCDD, the 2-position has higher reactivity than 1-position, but the difference is very small. From the distribution statistics of the intermediates during the reaction, we postulate that the steric effect plays an important role during the reaction and affect the dechlorination pathway of OCDD.     

陕西省山地日照时间的空间分布特征

基于100 m×100 m分辨率的DEM数据,根据太阳光线与起伏地形之间的几何关系,全面考虑坡度、坡向、地形遮蔽等地形因子对可照时间的影响,通过数值模拟,确定山区可照时间计算模型;同时利用常规气象站资料考虑大气对日照时间的影响,建立陕西省山区日照时间估算模型。采用交叉验证和个例年分析法进行模型验证,模型的精度和稳定性均较好。通过模型计算陕西省100 m×100 m分辨率各月可照时间、气候平均日照时间的空间分布。结果表明:局地地形对日照时间空间分布影响比较明显,山区可照时间与同纬度平地相比明显差异,表现出可照时间的非地带性分布特征;尤以冬季地形作用最显著;夏季影响最弱;同时年日照时间呈现出北高南低的空间分布特征,但局地地形因子的影响依然存在。最后详细探讨了坡度、坡向、地形遮蔽等因子对山区日照时间的局地影响规律。     

Shrinkage and fragmentation of grasslands in the West Songnen Plain,China

In the past century, especially the past five decades, the grasslands of the West Songnen Plain, Northeast China, were rapidly converted into croplands and salinized wasteland, and experienced a fragmentation process that is still ongoing. Almost no information is available on the spatial-temporal changes of grasslands in this area. In this study, grassland cover change, agricultural reclamation and salinized wasteland expansion were investigated during the past five decades. Grassland fragmentation was studied based on four landscape metrics. The grassland cover change was detected from a time series of topographic maps from 1954, satellite images of Landsat TM in 1986, 1995, and 2000 using remote sensing and geographic information systems (GIS). In addition, the land use changes were analyzed using a transition matrix of land use types, while the driving forces were explored according to climatic changes and socioeconomic developments. The results indicated a significant decrease in grassland area. Of the 1 418 945 ha of native grassland in 1954, approximately 64% was removed by 2000, while the number of patches (NP) increased from 865 to 2035 and the mean patch size (MPS) decreased from 1640 ha to 252 ha. During the whole study period, the average annual decrease rate of grassland was 34 894 ha/year. Cropland and salinized wasteland were the two main land use types into which grassland converted. During the past decades, obvious climatic changes occurred, which supplied a favorable potential environment for agricultural development but damaged grassland productivity. On the other hand, population, GDP and livestock number increased significantly as grassland quality decreased. According to the results, the shrinkage and fragmentation of grasslands may well be explained by socioeconomic development and aided by changing climatic conditions.     

浅谈生物资源平衡与生态平衡

地球是一个具有一定自洁、自我修复功能的大生态系统,它由各种植物、动物、人类、微生物有机的组成,维持着自然界的生态平衡。而大量的人类活动给地球的生态平衡产生了较大影响,特别是明显加快的城市化进程,使得这种平衡逐渐受到不可逆的破坏。论文重点分析了城市化给生态平衡所带来的问题,并由此提出了从生物链的角度建立生物资源平衡,从而实现新的生态平衡。将城市污染物的资源化和生态平衡联系起来,通过建立生物资源补充机制、改变城市垃圾和污水的处理方法等措施,促进生物资源平衡,在相对较大的范围内实现人类发展与自然相协调,实现可持续发展。     

基于主要污染物新增量的排污权指标来源研究

由于我国最初对环境资源的无偿使用,老企业占用了很多环境容量资源,导致排污权交易实施过程中出现指标来源困难的问题,致使很多建设项目无法获得排污权指标,阻碍社会经济发展.在分析排污权指标来源的基础上,提出了把污染物新增量作为排污权指标来源.把污染物新增排放量作为排污权的指标来源这不仅有利于明确总量控制下的排污权交易的指标量,更能提高各地排污减排的积极性和灵活性,还能缓解建设项目获取排污指标困难的现状.     

小飞蓬入侵对伊犁河谷草原土壤养分及活性有机碳组分的影响

因小飞蓬繁殖能力强,传播速度快,其入侵后排挤本土植物以较快的速度形成重度入侵群落,对草原生态系统的种类组成和群落结构产生影响.本文以伊犁河谷托乎拉苏草原内自然分布的猪毛蒿和糙叶矢车菊土著植物群落、混有少量小飞蓬的猪毛蒿和糙叶矢车菊轻度入侵群落、猪毛蒿糙叶矢车菊和小飞蓬中度入侵群落、小飞蓬重度入侵群落的4个群落为研究对象,采用样地实验的方法,研究小飞蓬入侵对土壤氮、磷、钾无机养分和活性有机碳组分变化的影响.研究表明,小飞蓬入侵后提高了土壤有机质含量.轻度入侵群落对土壤无机养分需求较大,明显降低土壤速效氮、速效磷、速效钾、硝态氮、铵态氮含量;随着入侵程度加深,逐渐恢复且均高于土著群落含量,其中速效氮含量增加不明显,重度入侵群落在0—10 cm、10—20 cm土层仍处于降低趋势.小飞蓬的入侵对于土壤活性有机碳组分影响较大.轻度入侵时降低土壤微生物活性、阻碍易氧化有机碳的积累,可溶性有机碳含量上升;小飞蓬重度入侵时对微生物量碳、易氧化有机碳含量的影响降低,并促进土壤微生物活性.     

Fe掺杂TiO2催化剂制备及其光催化脱汞机理

采用溶胶-凝胶法制备Fe-TiO₂(Fe掺杂纳米二氧化钛)催化剂,通过XRD(X射线衍射仪)、SEM(扫描电镜)、EDX(能量色散X射线光谱仪)和UV-Vis谱对其形态、结构、组成和性质进行表征. 采用Fe-TiO₂催化剂脱除气态Hg0(元素汞),研究了该催化剂在紫外光和可见光下的脱汞效果,并考察了Fe3+的最佳掺杂比. 结果表明:在Fe-TiO₂光催化剂中,TiO₂以锐钛矿相形态存在,当Fe3+掺杂浓度〔以n(Fe)/n(Ti)计〕达到0.010时,所制备的Fe-TiO₂在紫外光和可见光下的脱汞率均达到最大,分别为54.76%和18.92%. 提出了Fe-TiO₂光催化脱汞的可能机制:Fe3+掺入TiO₂结构中,使TiO₂的导带与Fe3+的d轨道发生重叠,导致TiO₂能带变窄,从而扩展了可见光的响应范围;Fe3+在TiO₂中作为一个浅俘获阱,当其俘获光生电子以后,光生空穴能够继续扩散到TiO₂表面发生表面化学反应,生成具有强氧化性的超氧自由基O₂-和·OH,对Hg0进行氧化;当Fe3+掺杂浓度大于0.010时,由于过多的Fe3+成为了光生电子和光生空穴的俘获位,从而使俘获的电子-空穴对通过量子隧道效应复合的概率增加,同时,活性氧化物种O₂-和·OH相互消耗,抑制了光催化效率.      

广州市不同功能区大气二噁英含量和分布特征研究

应用气相色谱-高分辨率质谱仪(GC-HRMS)对广州市秋冬季6个区域环境空气样品中的17种2,3,7,8-氯代二英含量进行了检测.结果表明,广州市各观测区域大气中二英毒性当量浓度范围为0.151～2.230pg.m-3,均值为0.418pg.m-3.各观测区域空气中二英毒性当量浓度分布存在一定的差异,本研究的背景区、居民住宅区和商业区二英毒性当量浓度较低且水平相近,分别为(0.294±0.099)、(0.305±0.115)、(0.308±0.102)pg.m-3.交通枢纽区、郊区和工业区二英毒性当量浓度相对较高,分别为(0.342±0.049)、(0.423±0.113)和(0.838±0.704)pg·m-3.广州市不同功能区二英毒性当量浓度呈现背景区<住宅区<商业区<交通枢纽区<郊区<工业区的分布特点.与2004年相比,广州市城区二英毒性当量浓度有所下降,郊区毒性当量浓度有所上升.