我国重金属防治与土壤修复行业2013年发展综述

综述了2013年我国重金属防治与土壤修复行业的发展环境、行业的技术发展进展,分析了我国重金属防治与土壤修复的市场规模和市场潜力,针对行业发展中存在的主要问题,提出了解决对策和建议,并对行业的发展进行了展望。     

我国地膜覆盖和残留污染特点与防控技术

地膜覆盖技术已成为我国农业应用最为广泛的农艺技术之一,但同时地膜残留污染也成为影响农业可持续发展的一个重大问题,系统分析梳理地膜覆盖种植技术、地膜残留污染的特点及防控技术对于该技术合理利用具有重要意义。本文在已有工作基础上,系统分析了我国地膜覆盖种植技术应用情况、地膜残留污染特点和防治技术。结果表明,20世纪80年代以来,我国地膜用量及覆盖面积一直呈大幅度上升态势,年增长率在8％左右,1991—2011年20年间,地膜使用强度增加了3～10倍,但存在明显区域差异。总体上,北方省区的地膜使用强度大,增长幅度快。地膜覆盖应用作物也从经济作物扩大到粮食作物,应用面积最大作物依次为玉米、蔬菜、棉花、烟草和花生等。地膜覆盖技术的应用产生了巨大效益,但同时也带来了一系列污染危害。长期覆膜农田土壤中都存在程度不同的残膜污染,残留量一般在71．9-259．1kg·hm-2。西北地区是残膜污染最严重的地区,土壤中残膜量远远高于华北和西南地区。残留地膜大小和形态多种多样,主要有片状、蜷缩圆筒状和球状等,在土壤中呈水平、垂直和倾斜状分布。目前,我国地膜残留污染防治技术滞后,人工回收是普遍和主要的回收形式,其他防治技术如机械回收、节约型地膜应用、生物降解地膜尚未较大规模应用。当前,为防止地膜残留污染进一步加剧,急需修订完善地膜标准和加强质量监管,提高可回收性;推广节约型地膜使用技术和残膜回收技术;开展地膜覆盖技术适应性研究,促进技术合理利用。     

延河沉积物的石油污染调查与分析

对延河干流和两条支流受石油污染河段的沉积物的取样分析结果表明 ,研究河段内的沉积物都不同程度的受到了石油污染。干流河段沉积物的石油污染负荷一般为 40～ 80mg/kg ,上游河段和污染支流汇入段负荷较高 ,平均为390mg/kg,最高可达 784mg/kg ;支流上的坪桥川和杏子河河段沉积物污染负荷为 6 0～ 2 5 0mg/kg。干流中下游及杏子河支流河段的污染沉积物主要来源于雨期流域表层污染土壤径流入河后的沿程沉积 ,而非雨期岸边油井的直接排污则是造成干流上游和坪桥川支流沉积物石油污染的主要原因     

氧和氮等离子体改性细旦涤纶的清洁工艺比较

该文对氧、氮低温等离子体改性细旦涤纶进行了研究,分别探讨了氧、氮等离子体放电参数对提高细旦涤纶上染率的影响,得出了2种工艺的最佳放电参数。实验结果表明:经氧、氮等离子体改性后,细旦涤纶的上染率分别提高了17%和5%,说明氧等离子体改性可显著减少印染废水中的污染物排放量,有利于环境治理,氮等离子体改性效果次之。      

Contamination of Oxygen-Consuming Organics in the Yellow River of China

Contamination of oxygen-consuming organics (OCOs) was one of the most serious problems in the Yellow River of China. This study was conducted to analyze monitoring of the data on OCOs contamination for the river in 1980 and during 1992–1999 as well as examining the effect of suspended solids (SS) on chemical oxygen demand (COD_Mn) and biochemical oxygen demand (BOD₅) of river water. Several significant results have arisen from the study. First, COD_Mn and BOD₅ of the river water showed an increasing trend from the upper to the lower reaches of the mainstream. BOD₅ values of river water in 1992 were significantly higher than those in 1980 and showed an increasing trend during 1992–1999. Second, OCOs in river water of the mainstream was attributed mainly to point sources; the ratio of point to non-point sources of BOD₅ was about 2.81. The load from point sources showed an increasing trend during 1992–1998. In contrast, the load from non-point sources manifested a decreasing trend during this period; this was caused by the decreasing trend of SS content in river water. The total load of BOD₅ from point and non-point sources displayed an increasing trend during 1992–1998. Third, as the humic substances in SS can hardly be biologically oxidized in natural conditions but can be oxidized by chemical oxidants such as potassium permanganate, COD_Mn was not suitable for being regarded as a parameter reflecting the pollution degree of OCOs in river water with a high SS content.     

Distribution of Iron, Manganese, Zinc and Atrazine in Groundwater in Parts of Palar and Cheyyar River Basins, South India

A study was carried out in a part of Palar and Cheyyar river basin to evaluate the current status of iron, manganese, zinc and atrazine concentrations, their origin and distribution in groundwater. Groundwater samples were collected during post-monsoon (March 1998 and February 1999) and pre-monsoon (June 1999) periods from 41 sampling wells distributed throughout the study area. The groundwater samples were analyzed for trace metals using AAS and atrazine using HPLC. The concentration of the trace elements in groundwater is predominant during pre-monsoon period. Distribution pattern indicates that the concentration of these elements increases from west to northeast and towards Palar river. Lower concentrations in the central part may be due to recharge of fresh water from the lakes located here. During most of the months, as there is no flow in Palar river, the concentrations of trace elements in groundwater are high. Drinking water standards indicate that Mn and Zn cross the permissible limit recommended by EPA during the pre-monsoon period. A comparison of groundwater data with trace element chemistry of rock samples shows the abundance of trace elements both in the rock and water in the order of Fe > Mn > Zn and Fe > Zn > Mn. This indicates that iron in groundwater is derived from lithogenic origin. Further, Fe, Mn and Zn have good correlation in rock samples, while it is reverse in the case of water samples, indicating the non-lithogenic origin of Mn and Zn. Atrazine (a herbicide) was not detected in any of the groundwater samples in the study area, perhaps due to low-application rate and adsorption in the soil materials.     

新疆平原区饮用地下水中F-含量的调查与评价

利用1997—1999年2058个饮用地下水中F-含量的测试成果。评价了新疆平原区饮用地下水中F-含量的状况,其结果为：F-含量变化范围为0．05—7．00mg/L,面积加权平均值为0．68mg/L,超标率18．9％。     

运用改进综合评分法筛选典型污染物的研究——以大武水源地地下水典型污染物筛选为例

结合潜在危害指数法和综合评分法筛选大武水源地地下水典型污染物。鉴于潜在危害指数法不考虑污染物的环境浓度,将潜在危害指数作为综合评分法的评价指标之一,同时引进污染物的检出频率、生物降解性、生物累积性、研究区是否有污染源检出、是否为环境激素、是否为美国环境保护署(EPA)优先有机污染物、是否为中国优先污染物、是否为持久性有机污染物等指标,计算不同污染物的综合得分,再通过聚类分析,筛选出典型污染物。研究结果表明,大武水源地地下水典型污染物为三氯甲烷、三氯乙烯、四氯乙烯、四氯化碳和苯。     

基于支持向量机的地下水质量综合评价

提出基于支持向量机（SVM）机器学习算法的地下水质量评价模型。首先给出了训练样本生成和数据规范化处理的具体方法,然后采用支持向量机的多分类算法构建模型,并使用k折交叉核实方法对参数进行验证优化。最后通过实证分析,并与单因子指数法、模糊综合评价法和BP神经网络法的评价结果对比分析可知,该方法简便易行,评价结果客观且准确度较高,具有很强的实用性。     

Recharge and Flow in the Medicine Lake Volcano–Fall River Springs Groundwater Basin,California

Isotopic measurements of the 34 m³/s discharge from the Fall River Springs of northern California indicate recharge from 50 km upgradient in high elevation regions of Medicine Lake Volcano. Age determinations suggest less than 20-year travel time. Data demonstrate Klamath Basin further north cannot be a recharge source. Mass balance calculations support that annual precipitation on the volcano supplies observed spring discharge, requiring 50%–75% recharge rates. Radiocarbon and δ¹³C of dissolved inorganic carbon indicate 30%–40% is derived from magmatic CO₂. Measured excess ³He is also consistent with the presence of magmatic gas derived from the Quaternary Age Medicine Lake Volcano.