长江经济带工业污染排放空间分布格局及其影响因素

长江经济带发展强调"不搞大开发,共抓大保护"战略,长江生态环境修复成为该地区发展的重要内容,因此探明长江经济带工业污染排放空间分布格局及其影响因素具有重要意义.选取2013~2017年长江经济带102个城市的工业SO₂、工业废水以及工业烟粉尘排放量作为基础数据,运用空间自相关分析和冷热点分析方法（Getis-Ord Gi^*）,揭示了长江经济带工业污染排放空间分布格局;采用对数平均迪氏分解模型（logarithmic mean Divisia index,LMDI）对长江经济带工业污染排放的影响因素进行分解.结果表明,2013~2017年长江经济带的工业SO₂、工业废水以及工业烟粉尘排放量呈降低趋势,高排放城市减少,低排放城市增多;各工业污染物随时间变化,空间关联程度增强;技术改善对工业污染排放有显著抑制作用,是影响长江经济带工业污染排放的最主要因素.     

基于景观格局的三峡库区生态脆弱性评价

三峡库区是我国的生态环境敏感脆弱区,进行生态脆弱性评价对于掌握其生态脆弱特征和识别生态环境问题具有重要意义. 基于遥感 (RS)和地理信息系统(GIS)空间分析技术,综合考虑景观格局和区域生态2类影响因素,进行三峡库区生态脆弱性评价. 结果表明:①景观类型中,脆弱度由高到低依次为水体、林地、旱地、草地和水田. ②景观破碎度与区域生态脆弱性之间的相关性显著,反映了人类活动对三峡库区生态环境的干扰剧烈. ③三峡库区生态脆弱区可划分为——Ⅰ区(0.171 500≤EVI＜0.191 225),Ⅱ区(0.191 225≤EVI＜0.210 950),Ⅲ区(0.210 950≤EVI＜0.230 675),Ⅳ区(0.230 675≤EVI≤0.250 400). 其中,Ⅲ区和Ⅳ区生态脆弱程度较高,主要分布在水域及其岸边带、高海拔区域和岩溶地貌区域. 特殊的地形地貌是三峡库区生态环境敏感脆弱的重要因素,而人类行为干扰是造成生态环境退化的决定性因子.      

辽宁省农用地质量空间分布格局及影响因素研究

采用GIS技术、地统计学分析和景观生态学方法对辽宁省农用地质量的空间分布规律及其多样性、均匀度、集中度、优势度等进行研究,结果表明：辽宁省农用地质量的区域分异明显,等别表现出由辽西低山丘陵区和辽东山地丘陵区向中部平原区的递增规律。探讨农用地质量空间格局的影响因素,发现农用地自然质量空间分布格局主要受到地带性因素与大尺度的非地带性因素的控制,农用地利用质量和经济质量空间分布格局受到人类活动的影响显著。     

不同空间配置的湿地植物群落对生活污水的净化作用研究

植物是湿地生态系统的重要组分,湿地湖滨植物群落物种组成和空间格局对湿地水体净化功能具有重要作用。选择茭草（Zizania caduciflora）、野菱（Trapa incisa）、金鱼藻（Ceratophyllum demersum）和蓖齿眼子菜（Potamogeton pectinatus）等4种云南高原湿地常见湖滨带植物物种,以不同配置方式分别构建4种不同植物群落：茭草-金鱼藻-金鱼藻（Z-C-C）、茭草-野菱-金鱼藻（Z-T-C）、茭草-蓖齿眼子菜-蓖齿眼子菜（Z-P-P）、和茭草-蓖齿眼子菜-金鱼藻（Z-P-C）,对不同植物群落净化污水的效果进行对比研究。结果表明：4种不同植物群落人工湿地对生活污水净化效果不同,经过Z-C-C群落处理后水体的COD降低率为（50.56±1.98）%,显著低于Z-T-C群落（69.66±4.15）%、Z-P-P群落（64.29±1.05）%,Z-P-C群落（66.67±1.13）%,（P〈0.05）;经过Z-T-C群落处理后水体TN降低率为（24.69±4.64）%,显著低于Z-C-C群落（53.29±0.71）%、Z-P-P群落（53.36±2.04）%、Z-P-C群落（54.44±0.29）%,（P〈0.05）;各群落对NH4＋-N去除率有显著差异（P〈0.05）,分别为（71.77±0.37）%,（67.22±0.53）%,（69.22±0.13）%,（80.85±0.31）%。研究表明：3种植物配置模式对生活污水的净化效果比2种植物配置模式的好;适当增加沉水植物的配置比例,可提高人工湿地对氮的去除效果;根系发达的植物具有更强的净化效果。     

程海冬季水华暴发期间氮、磷营养元素的形态与分布

氮、磷营养元素是湖泊生态系统中极其重要的生态因子,它们以不同形态存在于湖泊水体中,表现出不同的地球化学行为和生态效应,从而支配着湖泊生态系统的生产力水平和湖泊富营养化进程。通过设置3个断面9个采样站14个采样点,研究了程海湖水体中氮、磷营养元素的形态与分布,结果表明：2009年11月23日—2010年2月20日,以铜绿微囊藻（Microcystis aeruginosa Kutz.）为主的程海冬季水华暴发期间,总氮质量浓度0.540~3.906 mg.L-1,平均0.836 mg.L-1;总磷质量浓度0.036~0.166 mg.L-1,平均0.061 mg.L-1。其中,溶解态氮、溶解态磷分别为61.7%和50.8%。溶解态氮以有机氮为主,溶解态磷则以无机磷为主。水华期间生物可直接利用氮质量浓度0.118 mg.L-1;生物可直接利用磷质量浓度0.021 mg.L-1,分别占总氮、总磷质量浓度的14.1%和34.4%,显示出此特定时期,氮的消耗速度较磷快。氮素、磷素及其赋存形态在程海的时间分布上有不同的节奏;水平分布差异不明显;垂直分布在水表层至亚底层的水柱中差异也不明显,而在湖底层最高。     

生草栽培对三种岭南水果种植系统的生态经济影响评价

综合运用能值、经济与土壤生态学分析方法,以传统清耕模式为对照,定量研究了生草栽培对荔枝(Litchi chinensis Sonn)、龙眼(Dimocarpus longan Lour)和番荔枝(Annona squamosa Linn)三种岭南水果种植系统的生态经济影响。整合系统物质流、能量流和货币流,综合分析其自然资源基础、经济发展状况及可持续发展程度,并将土壤有机质的消耗纳入不可更新自然资源能值投入分析,为岭南水果业生草栽培与否提供科学依据。结果表明,生草栽培可以将荔枝和龙眼种植系统的能值可持续性从传统清耕模式的0.16和0.46分别提升到0.17和0.47;而使番荔枝种植系统的能值可持续性从传统清耕模式的0.59降至0.45。同时,生草栽培可提高荔枝和番荔枝种植系统的经济效益,而降低龙眼种植系统的经济效益。所有案例结果均表明,生草栽培可降低果园土壤有机质的消耗。     

Runoff and sediment losses from 27 upland catchments in Southeast Asia: Impact of rapid land use changes and conservation practices

Rapid changes in upland farming systems in Southeast Asia generated predominantly by increased population pressure and ‘market forces’ have resulted in widespread land degradation that has been well documented at the plot scale. Yet, the links between agricultural activities in the uplands and downstream off-site effects remain largely unknown because of the difficulties in transferring results from plots to a larger scale. Many authors have thus pointed out the need for long-term catchment studies. The objective of this paper is to summarize the results obtained by the Management of Soil Erosion Consortium (MSEC) over the last 5 years from 27 catchments in five countries (Indonesia, Laos, Philippines, Thailand, and Vietnam). The purpose of the study was to assess the impacts of cultivation practices on annual runoff and erosion rates. Initial surveys in each catchment included topography, soils and land use. Monitoring included climatic, hydrologic and erosion (total sediment yield including bed load and suspended sediment load) data, land use and crop yields, and farmers’ income. In addition, new land management options were introduced through consultations with farmers and evaluated in terms of runoff and erosion. These included tree plantations, fruit trees, improved fallow with legumes, maize intercropped with legumes, planted fodder, native grass strips and agro-ecological practices (direct sowing and mulch-based conservation agriculture). Regressions analyses showed that runoff during the rainy season, and normalized runoff flow coefficient based on erosive rainfall during the rainy season (rainfall with intensity exceeding 25 mm h⁻¹) increase with the percentage of the catchment covered by maize. Both variables decrease with increasing soil depth, standard deviation of catchment slope (that reflects terrain roughness), and the percentages of the catchment covered by fallow (regular and improved), tree plantations and planted fodder. The best predictors of sediment yield were the surface percentages of maize, Job's tears, cassava and footpaths. The main conclusions generated from this study were: (i) soil erosion is predominantly influenced by land use rather than environmental characteristics not only at the plot scale but also at the catchment scale; (ii) slash-and-burn shifting cultivation with sufficiently long rotations (1 year of cultivation, 8 years of fallow) is too often unjustly blamed for degradation; (iii) in its place, continuous cropping of maize and cassava promotes high rates of soil erosion at the catchment scale; (iv) conservation technologies are efficient in reducing runoff and total sediment yield at the catchment scale; (v) the adoption of improved soil management technologies by upland farmers is not a function of the degree of intensification of their farming system and/or of their incomes. The results suggest that if expansion of maize and cassava into already degraded upland systems were to occur due to increased demand for biofuels, there is a risk of higher runoff and sediment generation. A failure to adopt appropriate land use management strategies will result in further rapid resource degradation with negative impacts to downstream communities.     

高效絮凝菌的培养条件优化

从呼和浩特市污水处理厂筛选分离了1株高效絮凝剂产生菌YS2,通过培养条件优化试验确定了该菌株产絮凝剂的最佳培养条件:碳源为蔗糖、氮源为脲、N/C为2.5∶1、初始pH值为6.0、培养温度为30℃。絮凝试验表明:该菌株产生的生物絮凝剂对高岭土悬浊液有良好的絮凝效果,絮凝率达到95%。絮凝活性分布试验表明其絮凝活性全部存在于离心沉降物中,而上清液没有絮凝活性。16S rDNA测序鉴定其为克雷伯氏菌G。     

A Methodology Framework for Regional Land-use Change Studies based on Landsat TM images: A Case Study in Northeast China

Abstract

Land-use change is an important aspect of global environment change. It is, in a sense, the direct result of human activities influencing our physical environment. This paper analyzed the land- use change in Northeast China during 1985–2000 based on Landsat TM images. It divides Northeast China into five land-use zones based on the dynamic degree model of land-use: woodland/grassland-arable land conversion zone, dry land-paddy field conversion zone; urban expansion zone, interlocked zone of farming and pasturing and reclamation and abandon zone. The findings include the obvious increase of cropland area, paddy field and dry land increased by 75 and 276 thousand hm² respectively; urban areas expanded rapidly, areas of town and rural residence increased by 76.8 thousand hm²; areas of forests and grassland decreased sharply with the amounts of 1399 and 1521 thousand hm² respectively; areas of water body and unused land increased by 148 and 514 thousand hm² respectively. This paper also discusses the driving forces in each land-use dynamic zone and finds that some key biophysical factors affect conspicuously the conversion of different land-use types. The relation between land-use conversion and DEM, accumulated temperature (≤10°C) and precipitation was analyzed and represented. The land-use changes In Northeast China resulted from the changing macro social and economic factors and local physical elements. Rapid population growth and management changes can explain the shaping of woodland/grassland-cropland conversion zone. The conversion from dry land to paddy field in the dry land-paddy field conversion zone, apart from the change of physical elements promoting the expansion of paddy field, results from two reasons: one is that the implementation of market economy in China has given farmers the right to decide what and how they plant their crops, the other factor is originated partially from the change of the dietary habit along with the social and economic development. The conversion from paddy field to dry land is caused primarily by the shortfall of irrigation water, which in turn is caused by poor water allocation managed by local governments. The shaping of the reclamation and abandon zone is partially due to the lack of environment protection consciousness among pioneer settlers. The reason for the conversion from grassland to cropland is the relatively higher profits of farming than that of pasturing in the interlocked zone of farming and pasturing. In Northeast China, the rapid expansion of built-up areas results from two factors: the existence of a small number of towns and the huge potential for expansion of the existing towns and cities. The urban land expanded mainly in areas with a gentle topographic relief and low population density.     

Spatial-temporal analysis of wetland landscape pattern under the influence of artificial dykes in the Yellow River delta

The influence of anthropogenic activities,especially artificial dykes,on the coastal wetland landscape is now considered as a serious problem to the coastal ecosystem.It is important and necessary to analyze changes of coastal landscape pattern under the influence of artificial dykes for the protection and management of coastal wetland.Our study aimed to reveal the quantitative characteristics of the coastal wetland landscape and its spatial-temporal dynamics under the influence of artificial dykes in the Yellow River delta(YRD).It was analyzed by the methods of the statistical analysis of landscape structure,five selected landscape indices and the changes of spatial centroids of three typical wetland types,including reed marshes,tidal fiats and aquaculture-salt fields.The results showed that:(1)Reduction of wetland area,especially the degradation of natural wetlands,had been the principal problem since the dykes were constructed in the YRD.The dykes created conditions for the development of artificial wetlands.However,the new born artificial wetlands were still less than the vanished natural wetlands.(2)Compared with the open area,the building of artificial dykes significantly speeded up the changes of landscape patterns and the aggravation of the landscape fragmentation in the closed area.(3)The changes of area-weighted centroids of three typical wetland landscapes were greatly affected by dykes,and the movement of the centroid of the aquaculture-salt field was very sensitive to the dykes constructed in the corresponding period.