利用Rb/Sr值、有机碳氮同位素及14C重建贵州喀斯特地区古环境变化

本文利用碳酸盐岩风化剖面土壤中Rb/Sr值、有机碳氮的稳定同位素值(δ~(13)C_(org)和δ~(15)N_(org))并结合~(14)C定年结果,讨论了贵州黔西南喀斯特地区晚更新世以来的植被和气候变化情况。结果表明:(1)晚更新世以来,研究区气候在千年尺度上经历了多个冷热、干湿循环过程,植被以C4植物为主;(2)研究区在14 750 a BP时期可能发生过较为极端的气候事件;(3)Rb/Sr值和δ~(13)C_(org)值可以用来指示古环境变化情况,高Rb/Sr值和高δ~(13)C_(org)值指示湿热气候,低Rb/Sr值和低δ~(13)C_(org)值指示干冷气候。     

黔西南喀斯特地区红色风化壳的物源及元素迁移特征

南方喀斯特地区广泛分布着大量的红色风化壳,其成因及形成机制目前还存在争议。本文以贵州黔西南布依族苗族自治州泥凼石林的两处红色风化壳剖面(ND和YK)为研究对象,来探讨风化剖面上覆红土的物源问题,并计算其主、微量元素及稀土元素的迁移规律,认为本研究两处风化壳上覆红土为下伏基岩原位风化形成的,而且两剖面土壤均继承各自基岩的地球化学特征,并由于pH、风化强度等因素的影响表现出了元素迁移特征上的差异性。     

石化企业的节水与废水资源化问题

讨论了石化企业如何充分利用水资源，不断提高节水意识。并结合石化企业的具体情况，用系统工程的分析方法，深入研究节水和水资源化的方法和途径。对这些问题，提出一些看法供大家参考。     

Detecting forest landcape boundary between Mountain Birch and evergreen eoniferous forest in the northern slope of Changbai Mountain

Boundaries between different forest types in Changbai Mountain Eatern China are results from complex interactions between forest ecosystems,topogrphy,and geomorphology.Detecting and quantifying the transitional zones are highly important since high environmental beterogeneity and biodiversity are ofter found within these zpmes.In this study,we used GIS and multivariate statistics techniques(PCA and MSWA) to analyze data from Landsat TM satellite imageries and quantitatively determined the positions and widths of the landscape boundary betweeen mountain birch and evergreen coniferous forests in the northern slope of Changbai Mountain.The results showed that the widths of the landscape boundary ranges from 30-50 m while using the MWW A or/and PC method.Such detected widths are consistent with field transect data that suggest a 50m tranistional zone width.The results further suggest that TM data can be used in combination with GIS and statistical techniques in determining forest landscape boundaries.MSWA is more reliable than PCA,while PCA can also be used to determine the landscape boundary when transects are properly located.     

抓源头治理是落实“两控区”2000年初期目标的优先选择

针对我国煤中硫分赋存状况,抓源头治理,分别对高硫煤,中硫煤和低硫煤采取不同对策,切实有效地实现“两控区”２０００年的初期目标。     

农用土地价格评估——以新疆库尔勒市为例

根据农用土地的具体特征选择适当的方法和评估中具体的操作是本文探讨的重点。解决不同利用方式下农用土地收益差异的综合平衡计算是关键。结合库尔勒市农用土地分等定级的具体实践，建立一套较为完整的农用土地价格评估体系，为今后开展的工作提供范例。     

Experimental and simulated evaluations of airborne contaminant exposure in a room with a modified localized laminar airflow system

Environmental Science and Pollution Research - The traditional mixing ventilation is not an energy effective approach to remove indoor air pollutants, maintain breath zone air quality, and control...     

广西"十三五"环境保护和生态建设规划指标体系研究

生态环境保护目标指标是环境保护和生态建设规划中的核心内容,制定科学合理的规划指标体系,能够确保规划各项重点任务顺利实施.通过回顾分析"十一五"、"十二五"环境保护和生态建设规划指标体系,结合广西环境现状和发展趋势,在与国家和广西同期规划、计划、方案等衔接基础上,研究提出广西"十三五"环境保护和生态建设规划指标体系,设置了环境质量改善、总量控制、污染治理、风险防范、生态保护和生态公共服务等6个方面共29个指标,以期更好地指导"十三五"环境保护和生态建设工作.     

适用于中国燃煤电厂的汞监测及排放控制技术

随着GB 13223—2011《火电厂大气污染物排放标准》的颁布,汞排放问题正式列入了控制目标,这必将对燃煤电厂的环保设施提出新的更高的要求。在综述国外汞监测技术的前提下,总结脱硫脱硝污染物监测的经验,针对中国的具体情况分析了新形势下我国燃煤电厂汞监测技术的发展方向和关键技术的开发重点。同时分析了在最大化地利用燃煤电厂现有环保设施和设备的情况下,如何开发在今后一段时期内最适宜在我国广泛应用的汞排放控制技术,也对国内今后的政策发展进行了预测。     

Identification of key factors governing chemistry in groundwater near the water course recharged by reclaimed water at Miyun County, Northern China

Reclaimed water was successfully used to recover the dry Chaobai River in Northern China, but groundwater may be polluted. To ensure groundwater protection, it is therefore critical to identify the governing factors of groundwater chemistry. Samples of reclaimed water, river and groundwater were collected monthly at Chaobai River from January to September in 2010. Fifteen water parameters were analyzed. Two kinds of reclaimed water were different in type (Na-Ca-Mg-Cl-HCO3 or Na-Ca-Cl-HCO3 ) and concentration of nitrogen. The ionic concentration and type in river were similar to reclaimed water. Some shallow wells near the river bed had the same type (Na-Ca-Mg-Cl-HCO3 ) and high concentration as reclaimed water, but others were consistent with the deep wells (Ca-Mg-HCO3 ). Using cluster analysis, the 9 months were divided into two periods (dry and wet seasons), and all samples were grouped into several spatial clusters, indicating different controlling mechanisms. Principal component analysis and conventional ionic plots showed that calcium, magnesium and bicarbonate were controlled by water-rock interaction in all deep and some shallow wells. This included the dissolution of calcite and carbonate weathering. Sodium, potassium, chloride and sulfate in river and some shallow wells recharged by river were governed by evaporation crystallization and mixing of reclaimed water. But groundwater chemistry was not controlled by precipitation. During the infiltration of reclaimed water, cation exchange took place between (sodium, potassium) and (calcium, magnesium). Nitrification and denitrification both happened in most shallow groundwater, but only denitrification in deep groundwater.