珠江三角洲土地利用变化对特征大气污染物扩散的影响

在珠江三角洲两种下垫面条件下,应用CALPUFF大气污染扩散模式,对特征污染物SO2、SO42-的扩散进行数值模拟,探讨大规模土地利用变化,尤其是城镇建设用地增加,对珠江三角洲地区大气污染物扩散的影响,并通过对4个典型区污染物月均质量浓度变化特征分析,揭示土地利用变化对不同地区的污染物分布的影响机制。模拟结果表明：土地利用变化,尤其是城镇建设用地增加,不利于污染物扩散,污染源下风方向地区受影响较大,污染物质量浓度明显升高,SO2和 SO42-年均质量浓度分别增加14.07%和3.31%;受影响范围、变化幅度与污染源排污强度呈正相关,变化幅度亦与污染源距离远近呈负相关。土地利用变化后,尤其是城镇建设用地增加,四个典型区 SO2月均质量浓度都表现为升高趋势,且冬季 SO2质量浓度升高幅度最大,夏季升高幅度最小,临近污染源密集区的两个典型区SO2月均质量浓度分别增加33.6%和26.3%。土地利用变化不仅改变局地的污染扩散,也会对区域的污染扩散有一定影响,尤其对污染源分布密集区的大气污染物扩散影响强度最大。因此,建议人类在城市化建设过程中尽可能保留自然斑块,消除人工下垫面对污染物扩散的负面影响。     

A multi-scale approach to modelling spatial and dynamic ecological patterns for reservoir's water quality management

With growing levels of urbanization and agriculture throughout the world, it is increasingly important that both research and management efforts take into account the effects of this widespread landscape alteration and its consequences for natural systems. Freshwater ecosystems, namely reservoirs, are particularly sensitive to land use changes. In this context, modelling can be very useful, for decision support, as an investigative tool to forecast the outcome of various scenarios, to guide current management in order to meet future targets and to develop integrated frameworks for management accordingly to the Water Framework Directive (WFD). The present paper examined the applicability of a holistic Stochastic-Dynamic Methodology (StDM), coupled with a Cellular Automata (CA) model, in capturing how expected changes at land use level will alter the ecological status of lentic ecosystems, namely at physicochemical and biological levels. The methodology was applied to Portuguese reservoirs located in the Douro's basin and illustrated with a series of stochastic-dynamic and spatial outputs taking into account expected scenarios regarding land use changes. Overall, the simulation results are encouraging since they seem to demonstrate the tool reliability in capturing the stochastic environmental dynamics of the selected metrics facing spatial explicit scenarios. The ultimate goal was to couple monitoring assessment and the described modelling techniques to ease management and decision making regarding the practical implementation of the WFD, both at the scale of the reservoir body and at the scale of the respective river watershed dynamics.     

二氧化碳浓度升高对植物入侵的影响

从入侵植物和入侵植物群落两个方面,综述了大气二氧化碳浓度升高对植物入侵的影响。二氧化碳浓度升高,可以增加C3植物的入侵性,提高入侵植物的生物量、资源利用率以及繁殖能力,直接影响植物入侵;还可以通过改变土壤水分、氮循环、干扰体系等其它环境因子间接地影响植物入侵。此外,二氧化碳浓度升高,对入侵群落的初级生产量、组成与结构以及群落动态产生重要影响,改变群落的可入侵性。今后应当着重从群落水平,结合其它全球变化因子的共同作用研究二氧化碳浓度升高对植物入侵的影响,同时深入探讨其作用机制以及不同植物类群对二氧化碳的响应,为入侵种的预防和控制提供理论指导。     

环鄱阳湖区水足迹的动态变化评价

水足迹模型是计量水资源承载力的一个较新颖且日趋成熟的方法。水资源状况对鄱阳湖区生态系统的平衡、稳定以及生态系统良性循环有着重要意义。将水足迹模型运用于环鄱阳湖区进行实证研究,通过计量模型计算出环鄱阳湖区1989~2008年水足迹的时间序列值,并评价其承载状况。结果显示,近20 a来,环鄱阳湖区的水足迹需求由1989年的735亿m3增加至2008年的110亿m3,呈现出波动上升趋势。至今为止水足迹未超载,但盈余空间呈减少趋势。最后从优化水资源利用、倡导绿色消费和促进区域间贸易交流等降低水足迹的需求和增大水足迹供给的角度提出了提高水足迹承载力的对策。进而从水足迹的角度为环鄱阳湖区提高生态系统承载力提供理论依据,促进江西省鄱阳湖生态经济区的建设     

Research of the Response of Ecosystem to LUCC in Miyun County,Beijing: Based on Ecosystem Services Valuation

Abstract

Miyun County, located in the northeast of Chinese capital Beijing, was underwent remarkable variations in land use in recent years. This paper aimed to detect changes in land use of Miyun from 1997 to 2005, and to qualify the response of ecosystem to LUCC based on ecosystem services valuation. With two-periods TM images, we got land use change data, and then ecosystem services values were calculated using ecosystem services valuation coefficients proposed by Chinese scholar Xie Gaodi. Results showed that water area, farm land and unused land decreased while residential land, forest land, grassland and orchard land increased during the study period. The loss of ESV was RMB 206 million and the main reason was the decrease of water area and farm land area. As for spatial variation, there were most dramatically land use change and ESV decline in reservoir ecological protection region. The coefficient sensitivity analysis indicates that valuation coefficients used in the study are suitable and results are reasonable. The driving forces of ESV loss were rapid population growth and economic development. More work should be done to make eco-environment stay healthy.     

Fuelwood assessment at micro-watershed level in Northeast Himalaya:a case study in Manipur,India

Fuelwood is one of the major sources of energy in the domestic sector across the rural areas,especially in the developing regions across the world.The Northeastern Himalayan state of Manipur is dominated by the tribal population that largely depends on fuelwood from the nearby forest area.The entire dependence on forests for energy resources is affecting the sustainability of the forest ecosystem in the region,thus indicating the livelihood conditions.Since land-use land-cover change is the key driver to the change in resource availability of a region,the present study has tried to analyze the landcover changes over a period 28 years.The second major component affecting resource availability is the increasing population pressure that leads to changes in the land dynamics,which directly affect the resource production.Based on the existing consumption pattern,the total consumption of fuelwood in the watershed ranges fiom a minimum of 289.992 tons/year to a maximum of 3545.719 tons/year with an average of 1561.956 tons/year in the year 2009 and simulated fuelwood consumption for the year 2021 is around 1469.260 tons/year.Nine different probable scenarios of resource are proposed to calculate the stress value that can be used by the policy-makers and planners for suitable policy implementation at the micro level with a complex social system.     

基于3S技术的呼和浩特市土地利用／覆盖变化研究

本文以呼和浩特市为研究对象,利用遥感（RS技术）、地理信息系统（GIS技术）以及全球定位系统技术（GPS技术）——简称3S技术,对呼和浩特市2000、2004年遥感影像进行了综合技术处理,获得2期土地利用现状图,据此对呼和浩特市土地利用变化幅度及变化速度、土地利用变化程度、土地利用变化空间动态进行了分析,为区域土地资源科学管理及实现区域土地资源可持续利用提供科学依据。     

温室气体对气候环境的影响预测及其不确定性

随着温室气体排放量的增加,联系温室气体特有的保温效应,大气平均气温将升高。在采用气候模式对未来近百年的气候变化做出一定预测的基础上,分析未来可能出现的气候变化所造成的对气候环境方面的影响。详细分析了现阶段预测未来气候环境变化存在的不确定性,正是这些不确定性影响了预测的可信度。     

三峡库区汉丰湖水体氮磷及化学计量比季节变化特征

在分析2017年3月至2018年2月汉丰湖水体氮磷营养盐质量浓度季节性变化的基础上,利用氮磷化学计量摩尔比评估水体氮磷养分限制状态.结果表明:湖体TN、DN和NO₃^--N平均质量浓度分别为1.60、1.25和0.91 mg·L^-1,三者季节变化过程相似,均呈现出冬季最高、夏季最低的特点.NO₃^--N对水体TN贡献较大,NH₄⁺-N和NO₂^--N质量浓度维持在较低水平且变化平稳.TP、DP和PO₄^3--P平均质量浓度分别为0.13、0.09和0.06 mg·L^-1,TP和DP质量浓度变化相似,呈春夏季升高,秋冬季先降低再升高的趋势,而PO₄^3--P质量浓度则波动降低.TN/TP范围在11.07～56.02之间,均值为29.23,TN/TP呈季节性波动变化,最高值出现在冬季,最低值出现在...     

南亚热带土壤温度动态变化特征及其意义

根据定位系统观测资料,阐述了南亚热带山地常绿森林区、丘陵旱作区和平原水稻区多种土壤的温度变化与气温的关系。观测研究结果表明：低山常绿森林区温度的三维空间差异比丘陵区、平原区大,丘陵区又比平原区大;南亚热带林区的气温、地表温、30cm土温比中亚热带的高,比热带的低：南亚热带林区的谷地气温高于针叶林、混交林和阔叶林,谷地地表温低于针叶林而高于混交林和阔叶林,谷地20m土温低于针叶林、混交林而高于阔叶林;在气温一致的丘陵区栽植植物不同,其地表温、土温略有差异;在平原水稻土区,年气温、地表温、20cm土温差异不大,但30cm以下土温渐显差异;不同地貌单元的气温、地表温和土温的年际差异、年平均温度、各月及0～12～24时的温度动态变化各具特征。根据气温与植物生长的关系,拟把气温＞22℃的4～10月称热季、气温＜22℃的1～3月及11～12月称作凉季。可因地制宜,根据气温和土温的变化特征与土壤水分和作物生长的关系,采取措施调节温度,以利于作物生长。