大气CO2浓度升高对农田生态系统的影响

自由大气CO2浓度升高(简称FACE,即Free A ir CO2Enrichment)对陆地生态系统的影响是全球变化研究中的一个热点。综述了FACE条件下,农田土壤植物生物量质量变化和土壤微生物对植物的反馈作用,以及土壤痕量气体排放的趋势变化。     

山海关区农村生态环境状况及保护对策

从山海关区农村生态环境现状出发,客观分析了农村生态环境存在的水体污染、土壤污染、水土流失等问题,以及影响农村生态环境的主要因素,如污水和垃圾的无组织排放、化肥和农药的不合理使用、基础设施差、监管缺位等,提出应从环保体制、环保意识、基础设施建设、自然资源保护、污染防治、强化监管等方面采取切实可行的措施,保护农村生态环境。     

新时代我国土壤环境规划思路初探

在我国生态文明建设大背景下,土壤环境污染问题正受到广泛关注。如何通过规划手段加强土壤污染防控和管治,已成为学术界和管理部门的共同关注点。本文结合《土壤污染防治行动计划》和《土壤污染防治法》,对新时代土壤环境规划的基本概念和编制框架进行了探索,通过对土壤环境规划思路、基本内容、编制步骤等问题的讨论,为新时代土壤环境规划的深入开展提出建议,包括:加快健全土壤环境规划的规范和标准,为规划提供技术支撑;加强土壤环境规划的作用和地位,促进土壤环境规划与水、大气环境规划的融合;进一步完善土壤环境法律法规,构建土壤环境规划保障体系等。     

大麻茎腐病菌的分离及其对土壤环境影响的研究

从病变部位分离出两株病原真菌DN1和DN2,通过茵丝及孢子形态的观察,初步确定其分别为半知菌亚门链格孢属（Altemaria altemata）及轮枝孢属（M．Verticillium）。在pH值4～14之间,两株菌都能正常生长,对环境的适应能力较强。通过盆栽试验确定大麻对土壤pH的影响,结果表明大麻能修复弱碱性土壤。     

人类活动对土壤环境的影响及对策

人类不合理的开发行为给土壤环境带来了沉重的负面影响，主要表现为土壤沙化、土壤侵蚀、土壤盐渍化、土壤污染等。本文以此为出发点展开讨论，分析各种现象的成因，并提出相应对策。     

表土剥离对土地整治项目收益的影响研究

为了揭示表土剥离对土地整治项目收益的不同影响,作者采用采样分析、调查问卷、地统计分析、空间分析等方法对这种影响进行了分析。研究表明,表土剥离是土地整治工程必不可少的一步。通过土壤质量空间分布和作物投入一产出值比较分析,土地整治可有敬减少农业生产成本,而表土剥离可最大限度地保护土壤表层,通过追肥和田间管理,在2—3年时间可基本恢复耕地肥力。     

基于PSR模型的城市生态安全评价与贡献度研究——以铜川市为例

以铜川市为例进行城市生态安全评价和指标分析,采用压力-状态-响应模型和层次分析法构建出含有项目、因素、指标的铜川市生态安全评价体系。通过生态不安全指数定量表示城市的生态安全状况,对铜川市2014-2016年的生态安全状况进行了综合评价,并计算分析了各指标对城市总体生态不安全指数的贡献度。结果表明,铜川市的生态安全处于“临界安全”状态,并呈现逐渐向好的发展趋势。人均灌溉农田面积、地表水环境质量、环境空气质量和环保投资占GDP比例对铜川市生态不安全指数贡献度较大,应给予重视。     

以雨水为核心的城市水环境构建思路

在研究国内外利用雨水构建城市水环境的文献基础上,得出城市水环境构建要空中层、地表层和地下层综合构建三位一体的指导思想,以雨水为核心的城市水环境构建的思路是：从易到难,分步骤进行构建。     

Effects of Acidification and its Mitigation with Lime and Wood Ash on Forest Soil Processes: A Review

Anthropogenic acid deposition causes forest soil acidification and perturbation of the soil forming processes. The impact of soil acidification on tree growth is discussed in view of the role of mycorrhizal fungi in weathering and nutrient uptake. A review has been carried out of experiments involving treatments of forest soil by lime and wood ash, where soil properties and soil solution composition have been investigated. Results from these experiments in Europe and North America are summarized. In general, the content of C in the mor layer decreased as a result of treatment due to higher microbial activity and soil respiration as well as increased leakage of DOC. In addition, the content of N in the mor layer, in general, decreased after treatment and there are occasional peaks of high NO₃concentrations in soil solution. In nearly all reviewed investigations the pH of the deep mineral soil solution decreased and Al, SO₄and NO₃concentrations increased after treatment. These effects are probably due to the high ionic strength and increased microbial activity as a consequence of the treatments. In the soil, pH, CEC and base saturation increased in the upper horizons, but decreases in the upper mineral soil are also reported. In general, there was no increase in tree growth as a result of these treatments. The positive effects of the treatments on soil processes and tree growth are therefore questionable. In view of these conclusions, an investigation was carried out on the soil and soil solution chemistry and the role of mycorrhizal fungi in a spruce stand treated with two doses of lime and another treated with lime/ash in southern Sweden. The results of this investigation is reported in this volume.     

Comparison of Soil Extraction Isotherms of Soil Samples Saturated With Nonpolar Liquids

In multiphase systems capillary pressures play a significant role on fluid movement and retention. The facility to predict the effect of different thermal remediation strategies requires the knowledge of the effect of temperature on capillary pressure-saturation relationships in the soils. The objective of recent study was (a) to develop a technique for routinely measuring the pressure-saturation curves of soil samples saturated with a nonpolar liquid at different regulated temperatures (b) to build a database using the measured pressure-saturation curves and the physical, chemical properties of the model soils (c) to establish the dependence of nonaqueous phase liquid retention on the soil properties and the temperature. The retention curves (extraction isotherms) with nonaqueous phase liquid were determined using a modified pressure plate extractor. The wetting phase was a non-aromatic hydrocarbon distillation product. Pressure plates were designed and constructed in the laboratory of our department. The temperature was held constant at 20, 40 and 60 ^∘C. Statistical analysis was performed involving selected soil parameters and the measured nonaqueous phase liquid retention data. The results show that knowing some easily measurable soil parameters (bulk density, particle size distribution, humus and lime content) we can estimate the nonaqueous phase liquid retention of the soils. The measured “extraction isotherms” provide essential information about the temperature-dependency of pressure-saturation curves.