长三角快速城市化地区土地利用变化对生态系统服务价值的影响——以嘉兴市为例

基于浙江省嘉兴市1979~2012年的土地利用数据,评估了各种土地利用类型的生态系统服务价值,分析了30多年来嘉兴市土地生态系统服务价值的动态变化及其对土地利用变化和景观格局变化的响应。结果表明:(1)1979~2012年,嘉兴市建设用地面积变化最大,增加了136.6%,相应的耕地面积减少了15.5%。(2)1979~2012年,嘉兴市景观破碎度指数从0.6531上升到0.8762,随着城市化进程的加剧,耕地景观破碎度指数不断增加、聚集度指数减小。(3)1979~2012年,嘉兴市的总生态系统服务价值减少了14.7%,2000~2012年嘉兴市总的生态系统服务价值减少尤为显著,生态系统各单项服务价值整体也呈现下降趋势,耕地为嘉兴市提供的生态系统服务占嘉兴市总生态系统服务的70%以上。(4)运用相关分析方法对嘉兴市土地利用类型和景观格局对土地生态系统服务价值的影响分析表明,耕地和水域与生态服务价值呈正相关,而建设用地和未利用地与生态服务价值呈负相关;景观多样性指数(SHDI)和耕地破碎度指数与生态系统服务总价值呈显著负相关关系。     

Evaluating soundscape intentions in landscape architecture: a study of competition entries for a new cemetery in Järva,Stockholm

While soundscape is increasingly acknowledged within landscape planning and design discourse, there is little research that clarifies how soundscapes are actually dealt with in landscape architecture practice – partly owing to methodological insufficiencies. This paper, therefore, describes a model for evaluating soundscape treatment in landscape design proposals, focusing on three key aspects. With the dual aim of testing the model, and learning more about how soundscape is approached in practice, the paper spotlights a major design competition for a new cemetery in Sweden. The model proved fruitful and easy to apply. It showed that only limited attention was paid to soundscape in the competition as a whole, and was a useful means of pinpointing proposals where soundscape was fully considered as a design feature; one competition entry that did so is described in the paper. Discussions cover design practice, trends in the competition and model application.     

基于MSPA与MCR模型的余江县生态网络构建基于MSPA与MCR模型的余江县生态网络构建

在我国社会经济快速发展的背景下,城市化进程的不断推进导致城市生态斑块日益减少,生态环境问题正在逐年增加,构建生态网络是改善城市生态环境与服务功能的有效方法之一。以余江县为研究区,采用形态学空间格局分析(MSPA)方法和景观指数法,提取对生态网络具有重要意义的生态源地,并基于MCR模型构建综合阻力面,采用最小成本路径方法生成潜在廊道,再基于重力模型、中介中心度等对关键廊道及踏脚石斑块进行识别并提取,从而构建研究区潜在生态网络。结果表明：MSPA方法能够与MCR模型有机的结合,通过定量的分析识别出研究区潜在生态廊道,并根据斑块的中介作用选定踏脚石斑块,明确研究区景观要素的保护优先度,将景观中的潜在生态源地及廊道作为生态网络构建的主要依据,能够更加科学地为余江县生态网络的构建提供指导,同时也可为其他区域提供参考。     

工业搬迁区绿化带土壤铜污染及其在植物体内的迁移

老工业搬迁区主要道路两旁绿化带土壤由于历经老工业企业的变迁和环境的污染破坏,可在一定程度上对这一地区环境的历史变迁及重金属污染状况起到指示作用。采集沈阳铁西老工业搬迁区绿化带土壤及其绿化乔木和灌木植株样品,分析土壤中铜的总量及生物有效态含量,同时分别分析了绿化乔木(8种)和绿化灌木(6种)植株根、枝条和叶片的含铜量。结果表明,搬迁区绿化带土壤中含铜量为29.14~166.95mg/kg,显著高于沈阳市土壤铜元素的背景值;土壤有效态铜为0.23~1.72mg/kg,达到中等水平(0.3~1.0mg/kg)的占采样点总数的70.0%。数据还显示,绿化乔木和灌木对铜的蓄积能力依品种不同差异显著,同种植物不同部位(根、枝条和叶片)对铜的富集能力不同;总体上,绿化乔木植株体内含铜量的分布规律为根叶片枝条或叶片根枝条,绿化灌木植株体内含铜量的分布规律为根叶片枝条。对铜蓄积能力较强的绿化乔木为榆叶梅(Amygdalus triloba Lindl.)、垂柳(Salix babylonica Linn.)、旱柳(Salix matsudana Koidz.)和银杏(Ginkgo biloba),对铜蓄积能力较强的绿化灌木为大叶女贞(Ligustrum lucidum Ait.)、小叶女贞(Ligustrum quihoui Carr.)和紫叶小檗(Berberis thunbergii cv.Atropurpurea)。     

某1000 MW燃煤机组脱硝催化剂运行性能检测

以某1000 MW燃煤机组脱硝系统使用的脱硝催化剂为研究对象,分别对不同运行时间的催化剂进行了对比检测。检测结果表明,运行初期,催化剂表面沉积了一定量的碱金属,但属于正常范围内;没有出现过多的硫化合物的沉积;催化剂微观结构遭到一定程度的破坏,比表面积有下降趋势;催化剂机械强度基本保持良好;催化剂活性衰减在正常范围内,催化剂可以继续使用或添加加装层。     

2,4-D Mineralization in soil profiles of a cultivated hummocky landscape in Manitoba,Canada

The objective of this study was to quantify 2,4-D (2,4-dichlorophenoxyacetic acid) mineralization in soil profiles characteristic of hummocky, calcareous-soil landscapes in western Canada. Twenty-five soil cores (8 cm inner diameter, 50 to 125 cm length) were collected along a 360 m transect running west to east in an agricultural field and then segmented by soil-landscape position (upper slopes, mid slopes, lower slopes and depressions) and soil horizon (A, B, and C horizons). In the A horizon, 2,4-D mineralization commenced instantaneously and the mineralization rate followed first-order kinetics. In both the B and C horizons, 2,4-D mineralization only commenced after a lag period of typically 5 to 7 days and the mineralization rate was biphasic. In the A horizon, 2,4-D mineralization parameters including the first-order mineralization rate constant (k ₁), the growth-linked mineralization rate constant (k ₂) and total 2,4-D mineralization at the end of the experiment at 56 days, were most strongly correlated to parameters describing 2,4-D sorption by soil, but were also adequately correlated to soil organic carbon content, soil pH, and carbonate content. In both B and C horizons, there was no significant correlation between 2,4-D mineralization and 2,4-D sorption parameters, and the correlation between soil properties and 2,4-D mineralization parameters was very poor. The k ₁ significantly decreased in sequence of A horizon (0.113% day^?1) > B horizon (0.024% day^?1) = C horizon (0.026% day^?1) and in each soil horizon was greater than k ₂. Total 2,4-D mineralization at 56 days also significantly decreased in sequence of A horizon (42%) > B horizon (31%) = C horizon (27%). In the A horizon, slope position had little influence on k ₁ or k ₂, except that k ₁ was significantly greater in upper slopes (0.170% day^?1) than in lower slopes (0.080% day^?1). Neither k ₁ nor k ₂ was significantly influenced by slope position in the B or C horizons. Total 2,4-D mineralization at 56 days was not influenced by slope positions in any horizon. Our results suggest that, when predicting 2,4-D transport at the field scale, pesticide fate models should consider the strong differences in 2,4-D mineralization between surface and subsurface horizons. This suggests that 2,4-D mineralization is best predicted using a model that has the ability to describe a range of non-linear mineralization curves. We also conclude that the horizontal variations in 2,4-D mineralization at the field scale will be difficult to consider in predictions of 2,4-D transport at the field scale because, within each horizon, 2,4-D mineralization was highly variable across the twenty-five soil cores, and this variability was poorly correlated to soil properties or soil-landscape position.     

复合型絮凝剂处理景观水体

利用以生物絮凝剂(1 g/L MBF-28)与化学絮凝剂(5 g/L PAC)复配后的复合絮凝剂CBF28C处理景观水体,考虑了复配比、投加量、pH和投加顺序对处理景观水的影响。实验结果表明:对于反应体系为100 mL景观水体,当MBF-28与PAC溶液复配体积比为3∶1,反应体系pH为7.0,1 mL 1%CaCl2作助凝剂,1.5 mL CBF28C时,其絮凝效果最好,其COD,色度,TN,TP的去除率分别为90.7%,54.1%、46.6%和51.5%。最佳水力条件为:快速320 r/min,快搅时间45 s,慢速80 r/min,慢搅时间100 s。并且得出了前10 min内絮凝率的反应关系方程式。     

Soil type affects migration pattern of airborne Pb and Cd under a spruce-beech forest of the UN-ECE integrated monitoring site Zöbelboden, Austria

Anthropogenic trace element emissions have declined. However, top soils all over the world remain enriched in trace elements. We investigated Pb and Cd migration in forest soils of a remote monitoring site in the Austrian limestone Alps between 1992 and 2004. Large spatial variability masked temporal changes in the mineral soil of Lithic Leptosols (Skeltic), whereas a significant reduction of Pb concentrations in their forest floors occurred. Reductions of concentrations in the less heterogeneous Cambisols (Chromic) were significant. In contrast, virtually no migration of Pb and Cd were found in Stagnosols due to their impeded drainage. Very low element concentrations (<1 μg l⁻¹) in field-collected soil solutions using tension lysimeters (0.2 μm nylon filters) imply that migration largely occurred by preferential flow as particulate-bound species during intensive rainfall events. Our results indicate that the extent of Pb and Cd migration in soils is largely influenced by soil type.     

基于GIS的景观生态功能指标分析

针对当前我国规划及战略环评指标体系中缺乏直接反映生态功能指标的问题,提出可通过系统研究区域景观生态结构与景观功能变化间的关系,由斑块面积指数计算生物生产力、由景观香农多样性指数和景观香农均匀度指数反映生态质量,以此表征景观生态功能。以地理信息系统（GIS）为平台,提出了利用基于斑块面积而得到的景观要素转移矩阵及基于年鉴统计而得到的景观单位面积生物生产力的转移矩阵来计算生物生产力的方法,并在统计若干研究流域景观格局异质性指数文献的基础上发掘了景观多样性指数、景观均匀度指数与生态质量间的关系。最后,以江苏省沿江地区2000、2004年的数据开展了实例分析,结果表明,提出的生物生产力和生态质量这两个指标确实能反映区域景观功能的变化,在今后的规划和战略环评中具有一定的应用前景.     

长江流域常量元素的分布特征

2003年4月到5月对长江干流及主要支流河水中常量元素（Ca ²⁺,K⁺,Na⁺,Mg²⁺,Cl^-,SO^2-₄及碱度）进行了测定,并对常量元素的含量及影响因素进行了研究。结果表明,长江阳离子以钙为主,占阳离子总量的40%~80%;而阴离子主要为HCO^-₃,占阴离子总量的60%~90%;阴阳离子含量顺序为HCO^-₃>SO^2-₄>Cl^-,Ca ²⁺>Na⁺ >Mg ²⁺>K⁺。长江干流及主要支流河水的常量离子主要来自于岩石的风化,主要受碳酸盐类溶解的控制,硅酸盐类的风化过程较弱。而大气沉降的影响很小,只有SO^2-₄受大气沉降影响较大。长江干流的Na⁺、Mg²⁺、Ca²⁺、HCO^-₃和Cl^-主要来自于上游,下游只是对上游的简单稀释,而没有额外来源。与世界上其它大河相比,长江的常量离子浓度处于较高的水平;温带地区的河流河水中常量离子的含量常处于较高的水平;热带地区的河流河水中常量离子的含量相对较低。