坡岸截留强化处理设施在不同运行条件下对农业面源污染物去除效果

对坡岸截留强化处理设施在不同温度、不同雨强、不同降雨间隔条件下处理农业面源污染进行中试试验研究.结果表明,水温从20℃下降至4.3℃,COD、TN、NH+4-N、TP去除率下降了15.58%、48.93%、42.26%、57.75%;降雨强度由0.65mm·min-1增加1倍至1.30 mm·min-1,COD的平均去除率低了15.19%,TN、NH+4-N的去除效率相当,TP的去除效率提高了11.21%,但COD、TN、NH+4-N、TP单位面积去除的总量却提高了26.27%、68.3%、32.6%、104.2%;降雨间隔从2 d增加到4 d时对COD去除的影响不大,但使NH+4-N、TN的处理效率提高19.31%、13.95%,对TP的单位面积去除量提高71.43%,但去除总量有限.     

福建省地级市人为源活性氮排放及其特征分析

在人口增长和快速城市化的背景下,活性氮排放对生态环境的影响日益加剧.为研究省级尺度活性氮排放规律,采用排放因子法建立2000、2005及2010年福建省人为源活性氮排放清单,分析各地市3个年份活性氮排放量及排放强度特征.结果表明,3个年份福建省活性氮排放总量分别为538.4、587.0和619.97 Gg,呈整体增加趋势.在9个地级市中,增速最快的为莆田市,而漳州市排放量有所下降.排放量最大的为漳州和泉州,排放量最小的为宁德与厦门.从排放来源看,90%以上的排放来自农田生态系统和畜禽养殖系统.能源活动贡献较小,但其排放增长最为显著.2010年,各地市单位面积活性氮排放强度呈"东南沿海高西北内陆低"的格局,最高为厦门市,最低为三明市;GDP和人口排放强度则呈"东南沿海低西北内陆高"的格局,最高为南平市,最低为厦门市.在分析各地市活性氮排放源特征的基础上,探讨了不同地区活性氮减排重点,研究结果可为福建省及下辖各地市活性氮减排提供科学依据.     

苏鲁边界区域水资源保护与利用的协同机制探讨——以南四湖为例

通过对苏鲁界湖南四湖水源保护与利用状况的详细考察,全面系统分析了湖域水资源现状、存在的关键问题、影响因素等。针对湖域水资源现状,探讨了南四湖流域水资源保护与利用的协同机制,即建立湖域水资源协同规划与管理机制、湖区经济协同发展机制、生态修复与补偿协同机制、群众协同参与与监督机制、水危机协同处置机制和湖域界面冲突协同控制机制等,以促进跨界区域水资源的保护与利用,统筹区域协同发展,增强南四湖湖域的可持续发展能力。     

水体中甲基汞光化学降解特征研究

为探究水体中甲基汞（MMHg）的光化学行为,采用室内模拟实验,以不同波长紫外灯及室内可见光为光源,探讨紫外光波长、光强度等因素对MMHg光降解的影响,并根据生成物Hg0的量变化分析MMHg光降解反应历程.研究表明,MMHg光降解最终产物中含有Hg0,且光照条件对MMHg光降解速率、Hg0的产量有影响.在反应器暴露于紫外光条件下时,MMHg光降解速率随紫外光波长的变短而增加,随紫外光强度的提高而增加,且MMHg光降解呈一级动力学反应,速率常数分别为KUVA 0.403～0.562 h-1、KUVB 0.961 h-1、KUVC 1.221 h-1和KVL＋UVA＋UVB 1.346 h-1;Hg0释放通量为0.166～0.392 ng·min-1.当反应器暴露于可见光条件下时,反应器内MMHg浓度下降速率较慢,KVL0.061 h-1;Hg0释放通量为0.008 ng·min-1.而在黑暗条件下没有发现反应器内MMHg浓度下降,无Hg0生成.可见紫外光是导致MMHg降解的主要原因,光波波长与强度对MMHg的环境地球化学行为有重要影响.     

湄公河下游国家水质管理状况与区域合作前景

本文分析了老挝、缅甸、泰国、柬埔寨和越南等湄公河下游五国的水质状况及原因,通过汇总湄公河五国的水质管理法律法规及水质标准和介绍各国的水质管理措施,阐述了湄公河国家在水质管理方面做出的努力以及水质管理中存在的问题,并对湄公河国家在流域水质区域合作方面进行了展望。     

辽河流域水环境压力及污染治理模式研究

系统分析了辽河流域近十年社会经济和水污染物排放之间的关系,基于污染物排放强度和人均GDP指标,建立辽河流域COD和氨氮环境学习曲线;结合情景分析法预测在现有治污水平下,辽河流域未来水污染物排放趋势及水环境压力。结果表明,辽河流域水环境压力巨大。根据辽河流域污染治理中存在的实际问题,提出新时期的污染治理模式。     

Daytime light intensity affects seasonal timing via changes in the nocturnal melatonin levels

Daytime light intensity can affect the photoperiodic regulation of the reproductive cycle in birds. The actual way by which light intensity information is transduced is, however, unknown. We postulate that transduction of the light intensity information is mediated by changes in the pattern of melatonin secretion. This study, therefore, investigated the effects of high and low daytime light intensities on the daily melatonin rhythm of Afro-tropical stonechats (Saxicola torquata axillaris) in which seasonal changes in daytime light intensity act as a zeitgeber of the circannual rhythms controlling annual reproduction and molt. Stonechats were subjected to light conditions simulated as closely as possible to native conditions near the equator. Photoperiod was held constant at 12.25 h of light and 11.75 h of darkness per day. At intervals of 2.5 to 3.5 weeks, daytime light intensity was changed from bright (12,000 lux at one and 2,000 lux at the other perch) to dim (1,600 lux at one and 250 lux at the other perch) and back to the original bright light. Daily plasma melatonin profiles showed that they were linked with changes in daytime light intensity: Nighttime peak and total nocturnal levels were altered when transitions between light conditions were made, and these changes were significant when light intensity was changed from dim to bright. We suggest that daytime light intensity could affect seasonal timing via changes in melatonin profiles. Professor Dr. E. Gwinner died on 07 September 2004.     

不同雨强条件下太湖流域典型蔬菜地土壤磷素的径流特征

以太湖流域典型区域无锡市近郊区鸿声镇的蔬菜地为研究对象,采用人工模拟降雨的方法,通过野外径流小区试验,研究了不同雨强对菜地土壤磷素径流流失的影响.结果表明,初始产流时间随雨强的增大呈幂函数减小(R²=0.99),径流量在雨强较小时,缓慢上升,但随着雨强的增大急剧上升,在雨强0.83、1.17和1.67 mm·min^-1时,总磷(TP)和颗粒态磷(PP)都表现为初始流失浓度较高,随降雨历时延长略有下降,最终趋于稳定,而在大雨强2.50 mm·min^-1时,TP和PP呈现波浪式起伏,没有明显的变化趋势;在整个降雨-径流过程中,溶解态磷(DP)变化比较平缓,占TP的比例为20%～32%,而PP占TP的比例为68%～80%,其变化规律与TP相一致,由此可见,PP是土壤磷素流失的主要形态;通过对比不同雨强下不同形态磷素的流失率,发现TP的流失率,大雨强2.50 mm·min^-1是小雨强0.83 mm·min^-1的20倍,而DP的流失率,却是33倍,这表明随着雨强的增加,加速土壤PP流失的同时,也大大促进了DP的流失,主要原因是降雨前表施磷肥,使得磷肥中大量的无机态磷溶解释放到水环境中,增加了DP的流失,从而会加重受纳水体富营养化的程度.     

Elevated CO2 changes the moderate shade tolerance of yellow birch seedlings

To demonstrate the existence of light thresholds in plant growth and to examine the effects of elevated CO2 on the shade tolerance of a tree species, an experiment consisting of a completely randomized design for a total of 96 yellow birch (Betula alleghaniensis Britton) seedlings was conducted with 3 light levels (2.9%, 7.7%, 26.1% of full sunlight)×2 CO2 levels (350 and 700±10 ppm) with 4 replications in a phytotron. The study proved that thresholds exist and they vary in different plant organs. In ambient CO2, the thresholds were 13.3%, 18.7%, 15.0%, 15.2%, and 15.6% of full sunlight for stem, leaf, root, total plant biomass, and the averaged value, respectively. In 700 ppm CO2, the corresponding thresholds were 16.7%, 21.3%, 18.1%, 21.7% and 19.5% for stem, leaf, root, total plant biomass, and the averaged value, respectively. The lowest threshold in the stem is an indicator of the minimal light intensity for regular growth for seedlings of this species. Below this threshold, light-stressful growth occurs. The result of a paired t-test indicated that the thresholds in elevated CO2 were significantly higher than in ambient CO2. This suggests that yellow birch will lose its moderate shade tolerance, evolutionally becoming a shade-intolerant species, and that it may become more difficult to naturally regenerate in the future.     

Effect of platinum on the photocatalytic degradation of chlorinated organic compound

TiO2 nanoparticles, doped with di erent Pt contents, were prepared by a modified photodeposition method using Degussa P-25 TiO2, H2PtCl6 6H2O and methanol as the solvents. The physicochemical properties of Pt/TiO2 were investigated by the nitrogen adsorption and desorption isotherm measurement technique, X-ray di raction analysis and photoluminescence spectra, respectively. Reaction rates from photocatalytic removal of dichloromethane over Degussa P-25 TiO2 and Pt/TiO2 were evaluated. The average diameter and BET surface area of the TiO2 catalyst particles were 300 nm and 50 m2/g, respectively. The degradation e ciency was 99.0%, 82.7%, 55.2%, and 57.9% with TiO2 at inlet concentrations of 50, 100, 200, and 300 ppm, respectively. And the degradation e ciency was 99.3%, 79.7%, 76.5%, and 73.4% with a 0.005 wt.% Pt/TiO2 at inlet concentrations of 50, 100, 200, and 300 ppm, respectively. In addition, we found that the photoluminescence emission peak intensities decreased with increases in the doping amount of Pt, which indicates that the irradiative recombination was weakened. Furthermore, the results showed that the UV/0.005 wt.% Pt/TiO2 process was capable of e ciently decomposing gaseous DCM in air.