长江大保护5年来流域土地利用和生态系统服务变化

2016年我国开始实施长江大保护战略,防护林建设、港口码头整治、岸线复绿等一系列生态保护修复措施得以落实。以2010年、2015年、2020年3期遥感解译的土地利用数据为基础,对比分析前5年（2010—2015年）和后5年（2015—2020年）长江流域土地利用和生态系统服务变化,以及河湖滨岸缓冲带土地利用和港口码头分布变化,以考察长江大保护的成效。结果表明：1）2015—2020年,长江经济带6大城市群、重要保护区域及主要河湖缓冲区的土地利用转化主要表现为耕地和林草地转为建设用地。与前5年相比,长江流域生态系统综合动态度、生态用地变化指数和开发干扰指数都在下降,土地利用变幅与动态度都趋于平缓。2）2015—2020年,主要河湖缓冲区（0~5 km）的林草地、耕地和未利用地面积减少,湿地和建设用地面积增加。与前5年相比,河湖滨岸带港口码头总数量和总面积都由明显增加转为有所减少。3）2015—2020年,长江流域生长季植被覆盖度呈上升趋势。与前5年相比,高等级植被覆盖度面积持续增加,较低、中等和较高等级面积都持续减少。4）2015—2020年,生态用地面积与质量基本稳定。与前5年相比,生态系统服务综合当量由略有升高到保持稳定,变化趋于平缓。     

滨江城市水体污染的典型特征及保护对策

为保护和改善滨江城市水环境,以镇江为例调查了滨江城市水体污染的现状,认为滨江城市水在生活污染比重不断加重的情况下,存在着水质、水动力和泥沙交互作用的典型特征,提出要从控制污染、水量、泥沙3方面来保护水环境的对策建议。     

济南市“十三五”环境保护所面临的形势研究

随着我国经济发展进入新常态,"十三五"期间的环境保护工作也进入新阶段,为准确制定济南市"十三五"环境保护规划,文章对济南市经济总体发展情况,农业、工业和服务业发展情况,以及能源消费情况等方面进行了全面分析和预测,对"十三五"期间济南市环境保护工作面临的问题进行了识别,以期对济南市"十三五"环境保护所面临的形式做出全面准确的研判。     

中国滨海湿地现状及其保护意义

通过论述中国滨海湿地资源及其保护现状,分析了滨海湿地的生态效益、经济效益和社会效益以及红树林湿地和珊瑚礁湿地的作用,并提出了目前滨海湿地存在的问题及其保护的重要意义.     

新《环境保护法》的亮点、不足与展望

十二届全国人大常委会第八次会议表决通过了修订后的《环境保护法》,是中国环境法治建设的重要成就。新《环境保护法》与原《环境保护法》相比具有诸多亮点,如体现和贯彻了"保护优先"的理念,规定了生态保护红线制度、环境与健康监测调查和风险评估制度,明确了环境公益诉讼原告,规定了按日处罚制度。但也存在一些不足之处,如新《环境保护法》仍属管理法而非权利法、没有触及环境保护监督管理体制、环境保护法律体系缺乏合理协调、立法技术不够完善等。今后《环境保护法》的发展应注重从管理法向权利法转变、强化地方监管和建立区域性监管、协调环境保护法律体系。     

Field study of TCE diffusion profiles below DNAPL to assess aquitard integrity

An area where a free-product accumulation of trichloroethylene (TCE) dense non-aqueous phase liquid (DNAPL) occurs at the bottom of a 10-m-thick surficial sand aquifer was studied to determine the integrity of the underlying, 20-m-thick, clayey silt aquitard formed of glaciolacustrine sediment. TCE concentration-versus-depth profiles determined from aquitard cores collected at five locations indicated penetration of detectable TCE 2.5 to 3.0 m into the aquitard. Two of the profiles show persistent DNAPL at the aquitard interface, while two others indicate that DNAPL, present initially, was completely dissolved away producing concentration declines at the aquitard interface. The fifth profile suggests shallow DNAPL penetration (<0.5 m) into the aquitard, however, this penetration, which was likely caused by cross-contamination during core collection or cone penetrometry (CPT) of the aquitard interface, did not increase the maximum depth of TCE penetration. Combining the field profiles with one-dimensional model simulations, downward migration of the aqueous TCE front, defined as the EPA MCL of 5 microg/l, which was below the analytical detection limit, was projected to a distance between 4 and 5 m below the top of the aquitard. Using a single set of estimated aquitard parameter values, simulations of aqueous TCE migration into the aquitard provided a good fit to four of the field profiles with a migration time of 35 to 45 years, consistent with the history of TCE use at the site. These simulations indicate aqueous TCE migration is diffusion-dominated with only small advective influence by the downward groundwater velocity of 2 to 3 cm/year or less in the aquitard due to pumping of the underlying aquifer to supply water to the facility in the past 50 years. The applicability of the parameter values was confirmed by in situ diffusion experiments of 1-year duration, in which stainless steel cylinders containing DNAPL were inserted into the aquitard. The diffusion-dominated nature of the profiles indicates that the aquitard provides long-term protection of the underlying aquifer from contamination from this DNAPL zone. Simulations of long-term migration of the TCE solute front indicate breakthrough to the lower aquifer at 1200 years for the no advection scenario and at 500 years if the strong downward hydraulic gradient persists. However, even after breakthrough, the mass flux through the aquitard to the underlying aquifer remains relatively low, and when considered in terms of potential impacts to pumping wells, concentrations are not expected to increase significantly above present-day MCLs. The use of contaminant profiles of different time and distance scales, in addition to hydraulic data, dramatically improves the ability to assess aquitard integrity, and provides improved transport parameter values for estimating contaminant arrival times and fluxes. The apparent lack of deep preferential pathways for TCE migration, such as open fractures, is probably due to the softness of the silty aquitard deposit and minimal physical or chemical weathering of the aquitard provides long-term protection of the underlying aquifer from contamination from this DNAPL zone. Simulations of long-term migration of the TCE solute front indicate breakthrough to the lower aquifer at 1200 years for the no advection scenario and at 500 years if the strong downward hydraulic gradient persists. However, even after the breakthrough, the mass flux through the aquitard to the underlying aquifer remains relatively low, and when considered in terms of potential impacts to pumping wells , concentrations are not expected to increase significantly above present-day MCLs. The use of contaminant profiles of different time and distance scales, in addition to hydraulic data, dramatically improves the ability to assess aquitard integrity, and provides improved transport parameter values for estimating contaminant arrival times and fluxes. The apparent lack of deep preferential pathways for TCE migration, such as open fractures, is probably due to the softness of the silty aquitard deposit and minimal physical or chemical weathering of the aquitard.     

自然保护区生态旅游开发及保护规划探讨——以武夷山自然保护区为例

对自然保护区生态旅游开发意义和特点进行阐述，并以武夷山自然保护区为例，探讨如何制订自然保护区生态旅游保护规划，提出管理监控的内容和方法。     

齐齐哈尔市中心城区地下水开发与保护的探讨

简要说明了齐齐哈尔市中心城区地下水资源分布特征、地下水资源量、地下水补给与排放情况,根据地下水开采利用现状及存在的问题,围绕地下水水质,详细地探讨了改善与保护地下水资源的一系列有效途径。     

浅论农村生态环境的主要问题及其保护对策

农村环境质量不能得到改善，全国环境质量 难以改善。但长期来由于经济发展的压力和各咎人为破坏，工农业污染和自然损毁退化等，使农村生态环境问题十分突出，已成为区域可持续发展的严重制约因素，。许多贫困地区难以走上小康之路，生态环境经是重要原因之一。该文在概述了我国农村生态环境主要问题的基础上，着重报导致其恶化的主观原因，并提出了一些具体的对策措施。     

湖北网湖自然保护区生态质量评价

湖北网湖自然保护区属于内陆湿地和水域生态系统类型的自然保护区。根据网湖自然保护区的特征,通过选取自然性、多样性、稀有性、代表性、面积适应性、人类干扰、稳定性7个评价指标,运用指标赋分法和加权平均分法进行生态质量综合评价。结果表明,该保护区生态质量很好,气候适宜,动植物种类丰富,并且由于该区域目前经济处于初步发展中,人为干扰对其影响较小,因此短期内其生态环境质量会相对稳定,具有很高的保护和研究价值。同时针对网湖湿地目前所存在的威胁以及国家在治理和恢复其他湿地保护区的经验,提出了几点关于网湖湿地建设和远景开发规划的建议。