矿产资源经济区划的理论与方法

矿产资源经济区划是保护与合理开发利用矿产资源、实现资源优化配置和区域经济可持续发展的基础。本文依据经典的区位理论和地域分工理论,应用系统分析的方法,建立了矿产资源经济区划的一般程序,并归纳了定量分析中必要的技术手段和方法路线。     

我国矿产资源利用的环境问题及对策

矿产资源利用过程中靠成的环境问题是我国经济建设速发展所面临的一个现实问题本文全面地分析了矿产资源利用对环境影响的各个方面，分析了我国矿产资源环境问题的一些特点，提出了八个方面的对策建议。     

Utilization of red mud as catalyst in conversion of waste oil and waste plastics to fuel

The aim of this study was to investigate the possibilities of using a by-product (red mud) from alumina production as a catalyst for recovery of waste. The conversion of waste mineral oil (WMO) and waste mineral oil/municipal waste plastic (WMO/MWP) blends over red mud (RM), a commercial hydrocracking catalyst (silica–alumina), and a commercial hydrotreating catalyst (Ni–Mo/alumina) to fuel has been studied. The effect of the catalyst and the temperature on the product distribution (gas, liquid, and wax) and the properties of liquid products were investigated. In the case of hydrotreatment of WMO, the liquids obtained over RM at both 400° and 425°C had larger amounts of low-boiling hydrocarbons than that of thermal or catalytic treatment with hydrotreating catalyst. Gas chromatography and nuclear magnetic resonance analysis of the liquid products showed that RM had hydrogenation and cracking activity in hydrotreatment of WMO. In coprocessing of WMO with municipal waste plastics, temperature had an important effect as well as the amount of MWP in the blend and the catalyst type. The hydrocracking at 400°C produced no liquid product. In hydrocracking at 425°C, the product distribution varied with catalyst type and MWP amount. The commercial hydrocracking catalyst had more cracking ability in the conversion of WMO/MWP to liquid and gas fuel than RM. In the case of hydrocracking over RM, the largest amount of liquid having satisfactory quality was obtained only from the blend containing 20% MWP.     

略论清代自然资源的保护与利用

清代在水土资源、林木资源、矿产资源的保护与利用等方面采取了积极有效的措施，包括开垦土地、兴修水利、发展生态农业、植树造林、加强法制、设立环保机构等。     

WATER RESOURCES AND HUMAN HEALTH: THE VIEWPOINT OF MEDICAL GEOGRAPHY1

ABSTRACT: Medical geography studies both areal patterns of human health and disease and the environmental and cultural factors that contribute to such conditions. In such studies water resources are of major importance, not only because they are essential for life and their scenic beauty is of inspirational value, but also because they are involved, directly or indirectly, in more than 80 percent of all disease. The direct involvements result from various disease causing agents sometimes found in surface or ground water organic ones such as bacteria, worms, etc., which are known as pathogens, and inorganic ones such as trace elements and synthetic toxic chemicals. Surface waters may have indirect effects also, for they may serve as habitats or breeding places for organisms that do not themselves cause human disease but that serve as vectors or hosts for such pathogens. This paper will discuss these various roles of water resources in both endemic and epidemic disease occurrences and ways in which various human activities domestic, economic, recreational, or religious — increase or reduce our exposure to such diseases.     

地壳元素铁的吸光贡献对黑碳吸光增强估算的影响——以武汉为例

传统方法使用固定的波长吸收指数来估算地壳元素或棕碳吸光,但该方法只能处理仅存在两种组分的情形(黑碳/棕碳,或黑碳/地壳元素)的吸光贡献,存在较大不确定性.为此,本文提出一种新的方法,利用武汉在线观测数据(2021年2、3、8、9月),采用铁作为地壳元素的示踪物,利用最小相关系数法(MRS)得出地壳元素的吸光贡献,在扣除地壳元素吸光之后,再得到黑碳吸光增强系数(E_abs).结果显示观测期间370nm波段地壳元素吸光贡献均值为12.3%,月均值范围5.7%~15.5%,且波长吸收指数与铁的浓度正相关,表明地壳元素吸光贡献不可忽视.地壳元素吸光贡献呈现出显著的季节特征,呈现出冬季低,春季高的特点.地壳元素吸光的分离前后计算的E_abs存在一定的差异,受到了黑碳和铁的相关性的影响.观测期间扣除地壳元素吸光后,E_abs均值为1.43±0.53,在季节性上呈现春夏高,秋冬低的特性,春季较高E_abs值与春季黑碳较高的老化程度有关.E_abs对无机盐和有机物的含量存在正的依赖关系,证明了这些包裹物质对吸光增强的影响.     

生物质炭对华北平原4种典型土壤N2O排放的影响

生物质炭作为一种新型的土壤改良剂,在降低土壤温室气体排放方面发挥着重要作用.为明确生物质炭对冬小麦苗期土壤N_2O排放的影响,以华北平原的4种典型土壤(水稻土、砂姜黑土、褐土和潮土)为研究对象,进行田间试验,设置了4个处理:对照(CK)、单施化肥(NPK)、单施生物质炭(BC)和化肥与生物质炭配施(NPK+BC).结果表明,单施化肥显著增加了4种土壤N_2O排放,与对照相比,水稻土、砂姜黑土、褐土和潮土N_2O排放分别增加了314%、116%、240%和282%.添加生物质炭对华北平原4种土壤N_2O排放影响存在差异,与CK相比,单施生物质炭水稻土、褐土N_2O排放显著增加了72. 4%和50. 9%,而砂姜黑土和潮土BC与CK处理无显著差异.与NPK相比,生物质炭与化肥配施显著降低了4种土壤N_2O排放.添加生物质炭提高了4种土壤pH,其中,初始pH最低的水稻土,受生物质炭影响较显著,施肥则降低了4种土壤pH.砂姜黑土、褐土和潮土施肥处理N_2O排放通量均与铵态氮含量呈显著正相关,水稻土和砂姜黑土单施生物质炭处理N_2O排放通量与硝态氮含量呈显著正相关.     

Concentrations of inorganic elements in 20 municipal waters in Sweden before and after treatment – links to human health

The water chemistry of 20 municipal water treatment plants in southern Sweden, representing various bedrock situations, and water qualities, were investigated. Four water samples, raw and treated, were collected from each plant and analyzed by predominantly ICP-OES and ICP-MS at four occasions from June to December, 2001. The concentrations of Ca, Mg, K, Na, HCO₃ and a number of micronutrients, varied considerably in treated waters from the studied plants (ranges; Ca: 9.1–53.7 mg L⁻¹, Mg: 1.4–10.9 mg L⁻¹, K: 1.1–4.8 mg L⁻¹, Na; 5.4–75.6 mg L⁻¹, HCO₃: 27–217 mg L⁻¹). The elimination of Fe and Mn from raw water was efficient in all treatments investigated, giving concentrations in treated waters below the detection limits at some plants. Softening filters gave waters with Ca-concentrations comparable to the softest waters in this study. Adjustment of pH by use of chemicals like lye, soda or lime, modified the consumer water composition significantly, besides raising the pH. It was estimated that drinking water contributed to approximately 2.2–13% of the daily Ca uptake, if the gastrointestinal uptake efficiency from food and water was estimated to be around 50%. The corresponding figures for Mg was 1.0–7% and for F 0–59%. None of the studied elements showed any significant time trends in raw or treated waters during the follow-up period. The concentrations of potentially toxic metals such as Al, Pb and U were low and did not indicate risks for adverse health effects (ranges; Al: 0.5–2.3 μg L⁻¹, Pb: 0–0.3 μg L⁻¹, U: 0.2.5 μg L⁻¹).     

北京市大气PM2.5中矿物成分的污染特征

为了解北京市大气细粒子中矿物成分的浓度水平和污染特征,在清华园和车公庄进行了连续1a的PM_2.5累积周采样和全样品分析.Al、Si、Ca、Mg和Fe等地壳元素的周变化相似,最大周均浓度均出现在春季有强沙尘天气的一周;其季节变化显著,显示季节性的源排放以及气象条件对矿物成分的含量影响显著.土壤尘的季节平均浓度从夏季逐步上升,至次年春季达到最高(21.1 μg·m^-3),表明春季频繁发生的沙尘天气对土壤尘细粒子有重要贡献.大量的建筑活动可能大大增加了北京细粒子中Ca的负荷,应加强其排放控制.     

我国不同矿物气溶胶源区物质的物理化学特征

在我国不同的矿物气溶胶源区进行采样分析的结果表明,源区气溶胶物质的物理化学特性相差很大.黄土的颗粒最细,91%的黄土颗粒可以形成矿物气溶胶进行长距离输送;沙土较粗,只有15%的沙尘颗粒可以形成矿物气溶胶;2个煤灰样品的粒径差异较大,抚顺煤灰中＜74μm的颗粒高达39%,而呼和浩特煤灰只有7%.不同粒径颗粒的化学分析结果表明,微量元素在细颗粒上有较高的富集.黄土与沙漠土壤的细颗粒的化学性质十分相似,同煤灰的化学性质完全不同,其常量元素与A1的比值(E/Al)十分接近,而且与深海沉积物粘土中的比值(E/A1)