龙口市污水灌溉区农田重金属来源、空间分布及污染评价

采集龙口市污水灌溉区农田土壤,分析测定土壤pH和重金属含量,以采集的70个土壤样点为研究对象,根据多元统计中的相关分析和主成分分析探究研究区重金属的来源;采用地统计理论与GIS空间插值相结合的方法研究重金属元素的空间结构和分布特征;最后利用内梅罗指数法和改进的模糊综合评判法做重金属污染评价.结果表明,研究区内9种重金属元素在土壤中均有一定程度的富集,其中重金属Cd的均值是当地背景值的3.06倍,富集情况最为明显;指数法进行的污染评价显示Cu、Cd和Pb的综合污染指数分别为7.06、6.10和5.54,三者均属重度污染;相关分析和主成分分析结果显示,Cu、Zn和Pb、Cd主要受人为因素影响,污水灌溉是它们的共同污染因素,前两者为农业生产中化肥农药的过量使用与长时间的累积作用,而北部煤矿开采和煤矸石的堆积产生的污染以及电镀、机械制造等工业污染是后两者的污染来源;Co、Cr、Mn、Ni和As主要是受成土母质等自然因素的影响;据模糊综合评判的结果,研究区70个样点,有13个是中污染程度,23个属于轻污染,28个是警戒程度,6个样点处在安全范围内;从空间分布上看,重金属含量的高值区主要集中在黄水河下游的诸由观镇和徐福镇,说明污水灌溉给当地土壤造成了一定程度的重金属污染.     

中国耕地非农化压力时空格局的演变分析

社会经济和资源禀赋的区域差异导致耕地非农化压力表现出明显的空间异质性。开展耕地非农化压力测算并揭示其时空格局演变,是实现土地资源优化配置的基础。从经济因素、社会因素、产业结构和资源禀赋4个方面构建耕地非农化压力指数评价指标体系,采用熵值法计算各指标权重,继而计算1990~2014年中国31省的耕地非农化压力指数,并在此基础上开展了耕地非农化压力的时空格局分析。结果表明:(1)从空间格局分布来看,中国耕地非农化压力空间分布呈现明显的地理梯度,总体上呈现从东到西依次递减的态势。(2)从时间变化趋势来看,不同地区各省份之间的耕地非农化压力指数变化呈现多元化趋势。东部沿海地区,山东、浙江、江苏的耕地非农化压力指数处于上升阶段,上海、福建的压力指数变化趋势逐渐趋稳,广东的压力指数呈现下降趋势。中部地区,河南、河北、山西、江西的耕地非农化压力指数趋稳,陕西、湖北以及四川、重庆等西南地区省份的压力指数呈上升趋势。西部沿边3省(云南、西藏、新疆)的耕地非农化压力呈现了一致的下降趋势。(3)从时空格局结合来看,耕地非农化压力不同的省份其变化趋势呈现出截然不同的走向。在耕地非农化压力较大的地区,耕地非农化经历了从制度驱动向发展推动的阶段,经济增长的倒"U"型轨迹明显,经济增长与耕地非农化之间的关系逐渐脱钩。在耕地非农化压力居中或较小的地区,产业发展滞后,土地比较收益较低,耕地的社会保障作用、生态作用对耕地非农化的影响较大,从而增加了部分省份的耕地非农化压力。     

中国人口集疏格局与形成机制研究

人口集聚和疏散是人口空间分布格局最直观和最集中的体现,基于人口集聚度的中国人口集疏的空间格局和形成机制的研究,有助于准确把握中国人口空间分布的基本脉络,具有重要的学术价值和实践意义。研究采用了人口集聚度分级评价的方法,依据人口集聚度的不同,将各个地区划分为不同等级的人口集聚区,并对其分别讨论。在此基础上,结合中国人口分布格局、自然条件的空间分布格局、人居环境自然适宜性评价结果以及经济发展格局和城市化格局,对中国的人口集疏的空间格局进行了归纳,并进一步对相应的形成机制进行了探讨,得出了我国人口分布的空间不平衡日益加剧,并呈现沿海、沿江、沿线集聚的态势的基本结论,并对我国人口分布集疏格局的形成进行了探讨,提出了自然因素奠定我国人口分布的基本格局,而经济发展不平衡与城市化成为人口集聚的动力的观点。     

城市基本生态控制线划定范围研究

结合景观生态学原理,将城市基本生态控制线分解为基本农田控制线,河流与湿地控制线,林地控制线,山体控制线,海岸、沙滩控制线,针对每个景观生态要素控制线,通过定性、定量分析,分别提出划定依据、原则或方法。     

A2O-MBR工艺处理城市污Z作农业灌溉用水中试研究

为开发一种污水再生利用于农田灌溉领域的新型技术，本实验以城市污水为研究对象，采用A2O—MBR工艺进行中试研究，并将系统出水水质与《农田灌溉水质标准（GB5084—2005）》的主要水质指标进行对比分析。结果表明，系统COD和BOD，出水浓度范围分别为3．2～59．6mg／L、1．0～7．6mg／L，系统出水pH为7．16～7．54，悬浮物浓度几乎为0，上述指标均符合标准；TP、TN和氨氮的出水范围分别为0．03～0．79mg／L、1．6～17．7mg／L和0．8～10．3mg／L。《农田灌溉水质标准》没有对上述3个指标提出具体要求，且少量的氮磷是植物生长的营养元素。该系统出水的主要水质指标符合标准兽求．     

湖北宣恩七姊妹山天师栗(Aesculus wilsonii)群落特征

天师栗（Aesculus wilsonii）是我国特有的珍稀树种，其天然分布比较零散，极少有大面积的自然群落存在。对湖北宣恩七姊妹山天然分布的天师栗群落采用相邻格子法进行调查，研究了群落的物种多样性、空间格局、群落结构和种群径级结构等群落特征。结果表明：（1）天师栗是群落的主要优势树种，其重要值为22.7，远大于重要值排在第二位的红枝柴（重要值为13.7），且在群落中呈聚集分布类型；（2）群落物种比较丰富，相对于灌木层和草本层，乔木层丰富度指数和均匀度指数较低，优势度指数较高，说明乔木层物种没有灌木层和草本层多，且分布不均匀，但优势种作用显著，成层现象明显；（3）群落的年龄〖JP2〗结构显示，该群落虽然目前处于稳定阶段，但群落中5个优势种群的幼年个体补充都严重不足，潜在的影响群落以后的生存和发展。应采取保护措施，促进群落的自然演替.     

Metabolic diversity of the heterotrophic microorganisms and potential link to pollution of the Rouge River

The heterotrophic microbial communities of the Rouge River were tracked using Biolog Ecoplates to understand the metabolic diversity at different temporal and spatial scales, and potential link to river pollution. Site less impacted by anthrophogenic sources (site 1), showed markedly lower metabolic diversity. The only substrates that were utilized in the water samples were carbohydrates. Sites more impacted by anthrophogenic sources (sites 8 and 9) showed higher metabolic diversity. Higher functional diversity was linked to the physico-chemical and biological properties of the water samples (i.e. higher concentrations of DO, DOC, chlorophyll, and bacterial density). Biolog analysis was found to be useful in differentiating metabolic diversity between microbial communities; in determining factors that most influence the separation of communities; and in identifying which substrates were most utilized by the communities. It can also be used as an effective ecological indicator of changes in river function attributable to urbanization and pollution.     

SOIL WATER CHARACTERISTICS OF TWO SOIL CATENAS IN ILLINOIS: IMPLICATIONS FOR IRRIGATION1

ABSTRACT: Soil water was monitored by neutron scattering in six soils, three each within two drainage catenas in east-central Illinois, over a 15-month time span. The prairie soils have formed in: (1) 76–152 cm of silt loam, eolian sediments (bess) over glacial till (Catlin-Flanagan-Drummer catena), and (2) bess greater than 152 cm in thickness (Tama-Ipava-Sable catena). We characterized the water content of these soils over the total time span and for wet and dry climatic subsets, as an aid to potential irrigation decisions. Soils of the thin bess, C-F-D catena dried out to lower water contents and had greater soil water variability than did the thick bess soils. Under wet conditions, soil water contents in the two catenas were quite similar. Alleviation of surface and subsurface drying via irrigation would thus be more advantageous to yields on the C-F-D soils than on the T-I-S soils.     

IRRIGATION DEVELOPMENT AND MANAGEMENT ALTERNATIVES OF A DOLOMITE AQUIFER IN NORTHEASTERN ILLINOIS1

ABSTRACT: Irrigation development of the dolomite aquifer in eastera Kankakee and northern Iroquois Counties, Illinois, is extensive and increasing. Interruptions of domestic supplies have been reported with increasing frequency during the 1980's. To address this issue, a regional assessment of the ground-water resources of the region was conducted in 1987 and 1988. Options for managing the dolomite aquifer were also investigated. Hydrogeology of the dolomite aquifer was determined using five aquifer tests. Tranamissivity values of the dolomite aquifer ranged from 14,000 to 50,000 gpd/ft (168 to 600 m³/m/day). Storage coefficients were between 0.0001 and 0.0002, within the range of a confined (artesian) aquifer. Based on flow-net analyses, recharge of the dolomite aquifer ranged from 85,000 to 285,000 gpd/mi² (124.4 to 417.0 m³/day/km²). Water levels of the dolomite aquifer were mapped during five periods in 1987 and 1988 by measuring up to 226 wells completed in the dolomite aquifer. Maximum regional water-level declines because of irrigation pumpage were 44 feet (13.4 m) in 1987 and 72 feet (21.9 m) during the drought of 1988. Based on ground-water use data, precipitation records, and hydrogeologic information, the magnitude of water-level declines can be attributed more to differing hydrogeologic conditions than to pumpage or climatic changes. Existing ground-water management methods for resolving conflicts over the ground-water resources of the study area are reviewed and alternative management options explored.     

AGGREGATE MARGINAL RETURNS FROM WESTERN IRRIGATED AGRICULTURE1

ABSTRACT: Pressure is increasing in the western United States to reallocate water from irrigated agriculture to other competitive uses. Since water is normally allocated through water rights and not necessarily by the price system, the question of economic efficiency is a continual concern. Study results show that returns per acre-foot of water used in western irrigation are quite high and are closely tied to the livestock industry. Returns per acre-foot of water used for crops ranged from $60 to $1,500. When water was used to support livestock, returns per acre-foot ranged from $100 to $600. Clearly, losses of water supply that reduced irrigation production could also lower farm income significantly. Estimated returns also show what alternative uses would have to pay for water under competitive market conditions. Production elasticities are also shown for various states.