城市生活垃圾堆肥及垃圾专用肥对柑桔增产效应

城市生活垃圾堆肥及垃圾堆肥配制的专用肥对柑桔的肥效实验结果表明，垃圾堆肥作为基肥使用比常规施肥能使柑桔增产１２．４％－１４．５％，比空白对照增产７４．７％，施用垃圾专用肥的柑桔产量比常规施肥增产４．２％－５０．３％，比空白对照增产５８．４％－１２９．０％。施垃圾肥柑桔的营养成份（如维Ｃ，还原糖等）和常规施肥没有明显差异，也未发现重金属对桔子的污染。     

δC variations in tree rings as an indication of severe changes in the urban air quality

Annual growth rings sampled from three free-standing trees (Platanus hybrida sp.), grew in the metropolitan area of Palermo (Italy) and covering a 118 years time span (1880–1998), have been studied for their ¹³C/¹²C carbon isotope ratios. It has been found that the ¹³C/¹²C tree ring record, during the study time interval, decreased of −3.6‰, from −26.4‰ in 1880 to −30‰ in 1998. Such a progressive depletion has been attributed to the addition of anthropogenic ¹³C depleted carbon dioxide to the local atmosphere. The observed ¹³C/¹²C decrease has been used to infer some possible pathways of atmospheric CO₂ change in the study urban area.     

Impact of urbanization on hydrochemical evolution of groundwater and on unsaturated-zone gas composition in the coastal city of Tel Aviv, Israel

The coastal city of Tel Aviv was founded at the beginning of the 20th century. The number of its inhabitants and its water consumption increased rapidly. This study analyses a 15-year record (1934-1948) of pre-industrial development of groundwater chemistry in the urban area. Archive data on concentrations of major ions, dissolved gases (CO2 and O2), organic matter, and pH were available for each half-year during the period of 1934-1948. The major factors causing changes in the chemistry of groundwater flowing in three sandy sub-aquifers have been seawater encroachment due to overpumping, and infiltration of effluents from pit-latrine collectors. Influence of these factors decreases with depth. Landward-penetrating seawater passed through clayey coastal sediments, interbedded among sands and calcareous sandstones, and spread into the Kurkar Group aquifer. This has led to exchange of sodium (dominant in seawater) with calcium adsorbed on clay particles, enriching groundwater with calcium. Intensity of cation exchange decreases inland and with depth. Infiltration of pit-latrine effluents has introduced large amounts of ammonium into the unsaturated zone. Its rapid oxidation in unsaturated sediments has caused massive nitrate production, accompanied by pore-water acidification. This process induces dissolution of vadose carbonate, resulting in enrichment of groundwater recharge in calcium. Anthropogenically induced dissolution of calcite in the unsaturated zone has been the major factor for the increase of Ca2+ concentration in groundwater, accounting for about 80% of this increase. In the interface zone, an additional 20% of calcium has been supplied by cation exchange. Owing to pH increase caused by denitrification in the aquifer, Ca(2+)-rich waters supersaturated with calcite could be formed, especially in the capillary fringe of the uppermost sub-aquifer, which could induce calcite precipitation and ultimately lead to the cementation of sandy aquifers. Urban development has caused drastic changes in the gas content in the unsaturated zone and in groundwater. Carbon dioxide was intensively generated by nitrification-denitrification processes, by hydration of urea, to a lesser degree by oxidation of organic matter, and probably by anoxic biodegradation of organics. Between 1934 and 1948, concentrations of CO2 in unsaturated sediment air rose from 3.2% to 7.6%. In the unsaturated zone, oxygen consumption for oxidation of ammonium and organic matter lowered O2 concentrations in sediment air to unusually low values of 3.9-12.9%. Nitrification in the urban unsaturated zone could thus serve as a pump, sucking in atmospheric oxygen at a rate of about 0.3-0.5 g m-2 day-1. The extreme concentrations of CO2 and O2 in unsaturated sediments have been preserved due to production and consumption of gas under conditions of diminishing areas open to the atmosphere, uncovered by buildings and by roads.     

城市绿地降低空气中含菌量的生态效应研究

按照大气生物监测的方法和要求，选择了上海市区的交通干通。公园和居住区的主要类型的绿地，对绿地降低气挟菌数量的生态效应进行了初步研究，结果表明，绿地结构，植物种类配置和粉尘污染是影响绿地降低气挟菌数量效应的主要因素。     

城市垃圾能量估算方法探讨

本文根据Ｄｕｌｏｎｇ公式的计算结果，建立了根据城市垃圾组成的重量百分比估算城市垃圾能量的经验公式，并对它进行了检验。估算结果与Ｄｕｌｏｎｇ公式的计算结果进行相关分析，相关系数在０．９８以上，该经验公式具有较好的推广价值，用此公式对我国部分城市垃圾的能量进行了估算。     

主成份分析在城市生态经济动态评价中的应用

城市生态经济的动态发展过程,可以看作多种生态关系要素相互作用的集合沿时序轴波动的轨迹.在这种多变量分析中,完全采用人工筛选变量的方法难以避免确定权重等过程所带来的主观干扰.PCA(主成份分析)采用一种特殊的转换降维方法,根据原始数据自身的特点综合成几个主导因子,并最大程度反应原始数据的信息量.本文根据天津市四十年18项生态经济指标,采用相关矩阵和PCA双重筛选过程,得到载荷量大于90%的前三个主分量,将其作为天津市生态经济动态评价的基础.结果表明:天津市解放后四十年每十年一次的经济周期上迭加了自然社会等非经济因素的影响,表现出城市生态经济动态发展的三大阶段,这种发展主要受到宏观经济管理模式及其相应的投资机制的制约.     

中小城镇生活垃圾污染防治策略探讨

本文分析了我国中小城镇生活垃圾污染的现状和特征，本着因地制宜的原则提出了适合我国广大中小城镇垃圾污染治理的几个策略，其中的垃圾三类收集回收利用系统和建立在垃圾有效分选基础上的垃圾综合处理工艺是比较符合我国的国情，并在此基础上提出了中小城镇垃圾污染预防的几点建议。     

协调视角下长三角城市群的空间结构演变与优化

以城市群为主体优化城镇化空间布局是构建国土空间规划体系的重要内容,空间优化的本质旨在促进城市群内部大中小城市协调发展。以长三角城市群为案例,在测度2001-2016年长三角城市群26个城市的城镇化协调水平基础上,运用社会网络和多维尺度分析等方法,分析和识别城镇化协调关系及其空间结构和内在演变机理。结果表明：（1）随着长三角城市群的城镇化协调水平提高,城市群内部的高协调城市逐渐显现出以上海为核心的“Z型”分布态势,低协调城市则稳定分布在长三角城市群扩容后的范围;（2）根据城镇化协调水平的关联强度划分长三角城市群的凝聚子群,凝聚子群的加权平均中心度和联系密度增大后,上海极化效应更加明显;（3）从城镇化协调关系的空间和时间两个维度识别城市群空间结构,长三角城市群从在空间距离影响下以省会城市为中心的“圈层”结构,变形为在时间距离影响下的“核心—边缘”结构;（4）人口、土地和经济城镇化三者协调水平的变化影响着长三角城市群空间结构演变,相较人口与经济城镇化,土地城镇化对城镇化协调关系的加强具有显著促进作用。从协调视角剖析长三角城市群的空间结构并提出优化政策,有助于中国现有资源环境承载能力条件下城市群一体化建设和空间资源的高效利用。     

Assessing outdoor air quality vertically in an urban street canyon and its response to microclimatic factors

The vertical distribution of air pollutants in urban street canyons is closely related to residents’ health. However, the vertical air quality in urban street canyons has rarely been assessed using field observations obtained throughout the year. Therefore, this study investigated the seasonal and annual concentrations of particulate matter (PM_2.5 and PM₁₀), CO, NO₂, SO₂, O₃, air quality index, and their responses to microclimatic factors at three height levels (1.5, 27, and 69 m above street level) in an urban street canyon. The PM concentration was higher at 27 m than at 1.5 m in winter, whereas the situation was reversed in other seasons. It was found that photochemical pollutants such as NO₂ and O₃ were the primary pollutants in the urban street canyon. The days on which O₃ was the primary pollutant at the height of 1.5 m accounted for 81.07% of the entire year. The days on which NO₂ was the primary pollutant at the height of 27 and 69 m accounted for 82.49% and 72.33% of the entire year, respectively. Substantially higher concentrations of NO₂ and O₃ were found at the height of 27 m than at 69 m. In-canyon concentrations of NO₂ and O₃ were strongly correlated with air temperature, wind speed, and wind direction, which played important roles in photochemical reactions and pollutant dispersion.     

西安城市交通干道汽车污染物排放因子

在西安城市交通隧道内设３ 个空气监测点，对通过隧道的汽车排气形成的污染物浓度、隧道内风速、过往隧道的交通量进行采样、观测和统计。根据实测数据用大气扩散方程求得西安城市道路汽车平均单车 Ｃ Ｏ、 Ｈ Ｃ 和 Ｎ Ｏｘ 排放因子分别为３３２７９ ±１２１５８ 、３５７７ ±１８１６ 和４６０５ ±１９８１ ｍｇ／ｍ·ｖｅｈ 。与国外的成果相比，中国城市道路汽车 Ｃ Ｏ 和 Ｈ Ｃ 排放因子分别是国外发达国家汽车排放因子的２ ～９ 倍和３ ～９ 倍，而中国城市汽车 Ｎ Ｏｘ 排放因子约为发达国家汽车排放因子的二分之一。