三峡库区消落带土壤淹水过程中汞的释放及甲基化特征

为探索三峡库区消落带土壤淹水期汞的环境化学行为,利用模拟试验,设置A(15℃,低溶解氧(DO))、B(30℃,低DO)、C(15℃,高DO)3组处理,在人工气候培养箱中进行消落带土壤淹水过程中汞的释放与甲基化特征研究,淹水试验共进行了40 d.结果表明,淹水初期(0—10 d)土壤汞呈释放趋势,A、B、C等3组处理水体中总汞浓度逐渐增加,而土壤中总汞含量相应降低;随淹水时间的延长(10 d),二者达到平衡.淹水后,A、B、C处理上覆水甲基汞浓度随淹水时间的延长而升高,且分别在第15天、第8天、第15天达到峰值,第30天基本达到平衡;土壤甲基汞含量随淹水时间的延长而增高,并在第30天达到平衡,平衡时土壤及上覆水甲基汞浓度规律均表现为BAC.土壤-上覆水系统温度的适当升高利于土壤汞的释放及甲基化;高溶解氧利于土壤汞的释放,低溶解氧则更利于汞的甲基化.     

基于Z指数的昆明市洪涝研究

本文基于昆明市12个气象站点1963～2013年逐月降水量数据,采用Z指数的方法,得到旱涝等级评定结果,对昆明市洪涝的时空分布特征及成因进行了深入分析与研究,在此基础上提出防洪减灾对策.研究结果表明:时间分布上,昆明市在1963～2013年间,降水量经历了上升-下降-上升下降的波动状态,51年内共出现了8次重涝,3次大涝,10次偏涝,洪涝类型以重涝和偏涝为主,洪涝主要集中出分布在60年代中期至70年代中期、80年代末至21世纪初.空间分布上,昆明市的主城区昆明及其下风方向的嵩明地区降水较多,洪涝程度最为严重,呈贡、东川地区的降水较少,洪涝程度最轻.影响因素上,影响降水量最大的自然因素是相对湿度,其次是蒸发量及总云量;最大的人为因素是城市人口,其次是SO2排放量、建成区面积及道路面积.     

防治土壤污染应标本兼治

简要论述了土壤污染具有隐蔽、长期性和不易修复等特点,危害较大。针对土壤的危害,提出了防治对策。     

RIVERINE TRANSPORT OF NUTRIENTS AND DETRITUS TO THE APALACHICOLA BAY ESTUARY,FLORIDA1

ABSTRACT: The Applachicola River basin in northwest Florida covers an area of 3,100 square kilometers. Fifteen percent of the area is a dense bottomland hardwood forest which is periodically flooded. The annual leaf-litter fall from the flood-plain trees is a potential source of nutrients and detritus which eventually can flow into Apalachicola Bay. Transport of such material is dependent on the periodic inundation of the flood plain. The U.S. Geological Survey Apalachicola Rim Quality Assessment measured a total organic carbon flux of 2.1 × 10⁵ metric tons during the one-year period from June 3, 1979, to June 2,1980. Fluxes of total nitrogen and phosphorus during the same year were 2.1 × lo⁴ and 1.7 × lo³ metric tons, respectively. Flood characteirstics, such as prior hydrologic conditions, extent, and timing, are important in determining the amount and forms of materials transported. The 1980 spring flood produced a fourfold discharge increase over the annual mean outflow of 800 cubic meters per second. Nutrient concentrations varied little with discharge, but the 86-day spring flood accounted for 53, 60, 48, and 56 percent of the annual flux of total organic carbon, particulate organic carbon, total nitrogen, and total phosphorus, respectively. In 1980, the flood peaks, rather than the rise or recession, accounted for maximum nutrient and detritus transport.     

Coastal flooding, global warming and environmental management

A review of the difficulties associated with the definition of coastal flood frequencies and magnitudes leads to a recognition that there is considerable doubt in many parts of the world as to the precise nature of this particular hazard. Similarly, a review of the sea-level measurements that have been used to indicate a response to global warming shows that there is uncertainty about the amount of other controlling influences. What is clear, however, are that past management decisions about human endeavours in the coastal zone (including flood defences, occupance of flood-prone lands, extraction of ground water and natural gas) have had an impact on relative land and sea levels and have done more to increase the risk of coastal flooding than can be assigned so far to global warming. In addition, these changes induced by human activity may render inappropriate calculations of coastal-flood frequencies based on historical records since the latter relate to a period of time when the controls on flooding may have been very different.     

试论洪涝对水稻的影响

洪涝灾害是我国主要的农业气象灾害之一，水稻遭受洪涝灾害的概率较大，研究洪涝对水稻的影响具有重要的意义。通过现场试验，对水稻不同生长阶段遭受洪涝灾害的影响和不同温度下遭受淹浸后的影响进行了研究，并用数理统计方法对水稻遭受淹浸后，其产量的一系列变化作了定量的分析。     

重庆市的洪涝灾害管理

洪涝灾害是重庆市主要自然灾害之一,每年带来巨大的经济损失和人员伤亡,严重制约着重庆市社会、经济的可持续发展.本文在大量研究的基础上,分析了重庆市洪涝灾害的特点,总结了历年来的洪涝灾害及造成的损失,最后针对洪涝灾害的特点提出建立重庆市洪涝灾害管理系统,并对该系统作了详细分析.     

发展生态农业 实现农业持续稳定发展

我国是一个农业大国,具备生态农业建设的优势和特点,多年来在建设生态农业工程中,取得了经验,但还存在问题。必须提高生态农业规划目标,制定详尽的措施才能完成农业的持续稳定发展。     

Relative Influence of Streamflows in Assessing Temporal Variability in Stream Habitat1

Abstract: The effects of streamflows on temporal variation in stream habitat were analyzed from the data collected 6‐11 years apart at 38 sites across the United States. Multiple linear regression was used to assess the variation in habitat caused by streamflow at the time of sampling and high flows between sampling. In addition to flow variables, the model also contained geomorphic and land use factors. The regression model was statistically significant (p < 0.05; R² = 0.31‐0.46) for 5 of 14 habitat variables: mean wetted stream depth, mean bankfull depth, mean wetted stream width, coefficient of variation of wetted stream width, and the percent frequency of bank erosion. High flows between samples accounted for about 16% of the total variation in the frequency of bank erosion. Streamflow at the time of sampling was the main source of variation in mean stream depth and contributed to the variation in mean stream width and the frequency of bank erosion. Urban land use (population change) accounted for over 20% of the total variation in mean bankfull depth, 15% of the total variation in the coefficient of variation of stream width, and about 10% of the variation in mean stream width.