长江口沙洲表层沉积物磷的赋存形态及生物有效性

利用磷的连续分级提取方法,研究了长江口沙洲沉积物中磷的赋存形态分布特征,并探讨了沉积物中磷的生物有效性.结果表明,沙洲沉积物中总磷的含量为437.6～1103.7μg·g-1,其中79.5%以无机磷的形式存在,而无机磷中以碎屑态磷灰石磷为主;有机磷约占总磷的20.5%.磷的生物有效性分析结果显示,潜在的生物有效性磷主要包括弱吸附态磷、铁结合态磷和有机磷等3种赋存形态,而长江口沙洲沉积物中潜在的生物有效性磷含量较少,约为60.5～510.9μg·g-1,平均仅占沉积物总磷的28.86%.     

重庆长江广阳岛生态修复设计与实践探索

广阳岛的生态修复设计以"长江风景眼,重庆生态岛"为价值追求,聚焦"生态"和"风景".生态修复设计围绕"摸清本底、自然恢复、生态修复、增加生物多样性"四个核心方面展开,通过运用土壤改良技术、海绵理水技术和生态疏田技术等生态修复技术提升生态修复科技内涵,使生态修复后的广阳岛以生态为魂、以风景为象.一期按照四种模式完成生态修...     

长江经济带绿色城镇化效率评价及其影响因素——基于多维城镇化视角

本文引入资源和环境因素,以城镇化综合指数为期望产出,运用SBM方向性距离函数测算了2010—2020年长江经济带112个地级市（州）的绿色城镇化效率,并采用空间面板模型和地理探测器对绿色城镇化效率的影响因素进行实证分析。结果表明：长江经济带绿色城镇化效率整体水平不高,下游地区绿色城镇化效率高于上游和中游地区,资源消耗和环境污染是效率损失的主要来源;绿色城镇化效率表现出较为明显的热点—次热点—次冷点—冷点自东向西的带状分布格局,存在显著的空间正相关性。政府财政支出对绿色城镇化效率产生负向影响,外商直接投资和产业结构对提升绿色城镇化效率有显著的促进作用,且三者的影响具有地区差异性;市场力因素有利于绿色城镇化效率的提高。邻近城市间绿色城镇化效率的空间溢出效应明显,且空间溢出效应是长江经济带绿色城镇化效率空间差异的最主要因素,各因素的影响具有协同增强的作用。     

环境规制对城市生态技术扩散效率的影响研究

生态技术扩散是长江经济带生态文明建设的必要环节,也是企业履行环保责任的有效措施。本文以长江经济带110个地级及以上城市为研究对象,采用非径向方向距离函数对城市工业企业生态技术扩散效率进行测算,分别从整体和区域异质性角度实证分析环境规制对城市工业企业生态技术扩散效率的影响及内在机理。结果表明：长江经济带城市环境规制与生态技术扩散效率存在倒“U”形关系,环境规制对生态技术扩散效率还存在多重影响路径,外商直接投资和工业集聚在影响路径中分别起着中介作用,且外商直接投资和工业集聚的链式中介显著。在异质性分析中,发现环境规制、外商直接投资、工业集聚和生态技术扩散效率之间的关系因区域位置不同而存在差异性。为此,依据研究结论及环境规制实施现状提出相应的政策建议,实现长江经济带经济永续绿色发展目标。     

长江口区域水体半挥发性有机污染物健康风险评价

近年来长江口区域水体的有机物污染日渐严重.主要应用美国环境保护局(USEPA)的健康风险评价方法,并对其进行了一定的修改和补充,对长江口区域水体半挥发性有机污染物的健康风险进行了初步评价.结果表明:长江口区域水体半挥发性有机污染物的非致癌风险指数均小于1,其中单环芳香族类的非致癌风险值均在10-3数量级,卤代烃类的风险值在10-4数量级,均偏高于其他类物质;各类物质的致癌风险指数均在10-4数量级以下,其中六氯苯、双(2-氯乙基)醚和咔唑的风险指数相对较高,在10-5数量级.根据USEPA的建议值,初步认为目前长江口区域水体中单一半挥发性有机污染物不会对人体产生明显的健康危害.由于缺少相关的研究资料,因此各种有机污染物的联合健康效应评价尚无法进行.      

"十一五"脱硫计划实施前后长三角地区的硫沉降变化

采用RAINS ASIA模型研究了"十一五"期间长三角地区实施脱硫措施前后硫沉降超临界负荷的变化.结果表明,在90%保证率下,长三角地区硫沉降的临界负荷(以S计,下同)总值为78.38万t/a;2005年该地区硫沉降的超临界负荷总值为27.98万t/a,有45.6%区域面积的硫沉降超过临界负荷;如果不实施脱硫措施,到2010年长三角地区硫沉降超临界负荷的情景将急剧恶化,硫沉降超临界负荷总值将增长18.4%,超临界负荷的区域面积将增加到48.7%;"十一五"脱硫计划如期实施后,2010年长三角地区硫沉降超临界负荷总值将在2005年的基础上下降27.4%,但仍有39.1%的区域面积超过临界负荷,须采取更严格的措施控制硫沉降量.     

Nitrogen cycling of atmosphere-plant-soil system in the typical Calamagrostis angustifolia wetland in the Sanjiang Plain, Northeast China

The nitrogen (N) distribution and cycling of atmosphere-plant-soil system in the typical meadow Calamagrostis angustifolia wetland (TMCW) and marsh meadow Calamagrostis angustifolia wetland (MMCW) in the Sanjiang plain were studied by a compartment model. The results showed that the N wet deposition amount was 0.757 gN/(m2·a), and total inorganic N (TIN) was the main body (0.640 gN/(m2·a)). The ammonia volatilization amounts of TMCW and MMCW soils in growing season were 0.635 and 0.687 gN/m2, and the denitrification gaseous lost amounts were 0.617 and 0.405 gN/m2, respectively. In plant subsystem, the N was mainly stored in root and litter. Soil organic N was the main N storage of the two plant-soil systems and the proportions of it were 93.98% and 92.16%, respectively. The calculation results of N turnovers among compartments of TMCW and MMCW showed that the uptake amounts of root were 23.02 and 28.18 gN/(m2·a) and the values of aboveground were 11.31 and 6.08 gN/(m2·a), the re-translocation amounts from aboveground to root were 5.96 and 2.70 gN/(m2·a), the translocation amounts from aboveground living body to litter were 5.35 and 3.38 gN/(m2·a), the translocation amounts from litter to soil were larger than 1.55 and 3.01 gN/(m2·a), the translocation amounts from root to soil were 14.90 and 13.17 gN/(m2·a), and the soil (0-15cm) N net mineralization amounts were 1.94 and 0.55 gN/(m2·a), respectively. The study of N balance indicated that the two plant-soil systems might be situated in the status of lacking N, and the status might induce the degradation of C. angustifolia wetland.     

Distribution characteristics of dissolved organic carbon in annular wetland soil-water solutions through soil profiles in the Sanjiang Plain, Northeast China

Overwhelming evidence reveals that concentrations of dissolved organic carbon （DOC） have increased in streams which brings negative environmental impacts. DOC in stream flow is mainly originated from soil-water solutions of watershed. Wetlands prove to be the most sensitive areas as an important DOC reserve between terrestrial and fluvial biogeosystems. This reported study was focused on the distribution characteristics and the controlling factors of DOC in soil-water solutions of annular wetland, i.e., a dishing wetland and a forest wetland together, in the Sanjiang Plain, Northeast China. The results indicate that DOC concentrations in soilwater solutions decreased and then increased with increasing soil depth in the annular wetland. In the upper soil layers of 0-10 cm and 10-20 cm, DOC concentrations in soil-water solutions linearly increased from edge to center of the annular wetland （R^2 = 0.3122 and R^2 = 0.443）. The distribution variations were intimately linked to DOC production and utilization and DOC transport processes in annular wetland soil-water solutions. The concentrations of total organic carbon （TOC）, total carbon （TC） and Fe（II）, DOC mobility and continuous vertical and lateral flow affectext the distribution variations of DOC in soil-water solutions. The correlation coefficients between DOC concentrations and TOC, TC and Fe（II） were 0.974, 0.813 and 0.753 respectively. These distribution characteristics suggested a systematic response of the distribution variations of DOC in annular wetland soil-water solutions to the geometry of closed depressions on a scale of small catchments. However, the DOC in soil pore water of the annular wetland may be the potential source of DOC to stream flow on watershed scale. These observations also implied the fragmentation of wetland landscape could bring the spatial-temporal variations of DOC distribution and exports, which would bring negative environmental impacts in watersheds of the Sanjiang Plain.     

长江中下游湖泊保护和管理的若干建议

长江中下游地区是我国面向21世纪的经济重地,长江是我国唯一具有全国意义的战略水源地,是我国水资源供需平衡的最后防线。然而在自然演化宏观背景下,流域经济的高速发展,大规模开发利用等人类活动的强烈影响,引发了一系列负面环境效应。湖泊湿地生态环境被破坏问题严重,突出表现在生态调节和自我恢复功能大幅度降低,并已造成了严重的生态后果,危及长江水系的生态平衡,影响了区域经济的可持续发展。在大量野外考察和调查基础上,针对长江中下游湖泊湿地当前的生态环境状况及存在的问题,提出了若干对策和建议。     

大型水利水电工程实施占用耕地补偿制度的思考

本文在分析长江三峡工程用地特点的基础上。对大型水利水电工程实施耕地补偿制度中的问题和困难进行调查研究，认为应从新的视角来认识大型水利水电工程的耕地占补平衡问题。进而探索耕地补偿制度实施的新途径和新方式。应在耕地总量动态平衡政策适当调整的基础上．将“以地补地”和“缴费补地”的方式相结合。既通过土地整理．在提商土地质量的前提下增加耕地的有效面积：又要落实耕地开垦费．扶持库区的土地整理。从而使库区的耕地占补制度顺利实施。