浙江沿海地区新农村住房设计研究初探——以台州玉环县为例

该文通过对台州玉环县新农村住房设计进行总结,归纳了目前浙江沿海地区新农村住房设计的特点和形成的制约条件,并探讨了如何针对这些制约条件有效的展开住房设计,总结了一套研究方法,最后结合这次住房设计实践提出了一些关于新农村住房设计的思考。     

浅析章水流域“7.3”特大洪灾

通过对江西省章水流域大余县＂7.3＂特大洪灾抗洪救灾工作进行全面总结和深入分析,对今后的防汛抗洪工作提出思路和建议.     

石阡县石漠化现状及治理对策的探讨

通过对石漠化成因的分析及对石阡县石漠化现状和危害情况的阐述,得出造成石阡县石漠化的深层原因及相应的治理对策。     

Geochemical modeling of groundwater in southern plain area of Pengyang County,Ningxia,China

The purpose of this paper iS to examine the evolution mechanisms of a hydrochemical field and to promote its benefits to the living standards of local people and to the Iocal economy in the southern plain area of Pengyang County,in Ningxia,China.Based on understanding of the hydrogeological conditions in PengYang County,the chemical evolution characteristies of groundwater in the plain area were analyzed.PHREEQC geochemical modeling software was used to perform hydrochemical modeling of water-rock interaction and to quantitatively analyze the evolution processes and the formation mechanisms of the local groundwater.Geochemical modeling was performed for two groundwater paths.The results showed that,along path 1,Na+ adsorption played the leading role in the precipitation process and its amount was the largest,up to 6.08 mmol/L;cation exchange was significant along path 1,while along simulated path 2,albite accounted for the largest amount of dissolution,reaching 9.06 mmol/L,and the cation exchange was not significant.According to the modeling results,along the groundwater flow path,calcite and dolomite showed oversaturated status with a precipitation trend.while the fluorite and gypsum throughout the simulated path were not saturated and showed a dissolution trend.The total dissolved solids(TDS)increased and water quality worsened along the flow path.The dissolution reactions of albite,CO2,and halite,the exchange adsorption reaction of Na+,and the precipitation of sodium montmorillonite and calcite were the primary hydrogeochemical reactions,resulting in changes of hydrochemical ingredients.     

宜阳县矿山地质环境恢复与综合治理规划研究

为了最大限度地解决采矿活动引发的地质环境问题、避免造成地质环境恶化、消除地质环境隐患,使已破坏的矿山地质环境得到有效的治理,基于矿产资源概况及矿产资源开发利用现状,分析了矿山地质环境现状与发展趋势,得到了矿山地质环境问题、矿山地质环境破坏现状、恢复治理的矿山地质环境现状以及矿山地质环境发展趋势;研究了矿山地质环境综合治理规划,制定矿山开采准入条件、优化资源开采布局、实行矿产资源规模化开采、调控开采总量、提高资源综合利用率等政策措施,强化矿产资源开发准入时对地质环境的源头保护作用。最后,分析了矿山地质环境恢复治理工程部署。研究能够有效的保护矿山地质环境,使矿山成为真正的绿色矿山,基本消除了由于矿山开采带来的环境、地质方面的影响,使周围的群众能够正常的生产、生活,对全社会的安定团结和稳定发展也有重要意义,是保证矿区区域可持续发展的重要组成部分,具有重要的社会效益。     

阿克塞县水泥用石灰岩矿地质环境特征及生态环境修复治理研究

矿山目前处于露天开采状态,由于多年的粗放式,对原有地质环境造成了严重的破坏。为了实现矿产资源的可持续发展,通过对阿克塞县水泥用石灰岩矿地质环境和土地利用现状调查,发现地质环境问题主要为发育不稳定斜坡和土地损毁情况,其中损毁土地面积共计246.87 hm2,并开展了矿山地质环境现状评价和土地复垦方法讨论,最大限度地减轻矿业活动对矿山地质环境的不利影响,实现矿山地质环境的有效保护与恢复治理,使矿山企业在开发矿产资源的同时,保护土地资源、恢复生态环境,促进人与社会和谐发展。     

《十排考》——清末香山盐场社会的文化记忆与权力表达

本文以清末《香山翠微韦氏族谱》所载《十排考》一文为研究对象,考察明清香山盐场的社会变迁,诠释食盐专卖制度下食盐生产与地域社会的互动。明初灶户立籍,香山盐场的盐民获得了合法的社会身份。明代中期以后,伴随着沙田的成长,适宜食盐生产的海水逐渐淡化,导致盐产下降,灶丁逃亡,黄萧养之乱加快了这一过程。香山社会经济格局重新整合。清代以后,香山盐场的盐业生产已经衰落,生产中心转移至三灶。原香山场的族群对市场、宗族、民间信仰、科举等文化和权力资源的操控,揭示出市场与社会文化、地方政治之间的复杂关系。     

Rare Earth Elements Compositions and Genesis of Xinhua Large-Scale Phosphorite Deposit in Western Guizhou, China

Zhijin County in Western Guizhou is one of the most important production areas of phosphorites in China. In order to investigate genesis of the phosphorites, their REE compositions were analyzed by using inductively coupled plasma emission mass spectrometry (ICP-MS) method. For comparison, phosphorites from the Lower Cambrian black rock series in Southern China, such as Zunyi in Guizhou and Zhangjiajie in Hunan Province, were also analyzed. The analytical data show that: (1) Xinhua phosphorites possess a quite high and greatly varied total rare earth elements (ΣREE), which varying between 164.23×10-6 and 1395.01×10-6 with average of 642.54×10-6, remarkable differentiation between light (LREE) and heavy rare earth elements (HREE), and the ΣLREE/ΣHREE ratios varying between 5.04 and 6.52. The ΣREE and ΣLREE/ΣHREE ratios of the Zunyi and Zhangjiajie phosphorites are 156.69×10-6～637.41×10-6 with average of 431.75×10-6 and 3.17～6.95 with average of 4.37 respectively; (2) All the phosphorites from Xinhua, Zunyi and Zhangjiajie show remarkable negative Ce anomalies. Besides, the Xinhua phosphorites possess lower δCe, which varying between 0.26 and 0.53 with average of 0.35, while δCe of the Zunyi and Zhangjiajie phosphorites are 0.30～0.66 with average of 0.47, suggesting that all of the phosphorites are typical marine sediments deposited mainly in ancient peri-continental seas, and the depositional position of the Xinhua phosphorite might be deeper; (3) Most phosphorites from Xinhua, Zunyi and Zhangjiajie possess unremarkable positive Eu anomaly, and only a few of samples show obvious ones. The δEu varies between 0.98 and 2.4, suggesting that hot (>200 ℃) and strong reductive hydrothermal fluids might have been involved in genesis of the phosphorites; (4) The Xinhua phosphorite is relatively depleted in HREE, and LaN/NdN and δY of most samples are >1 and >1.5 respectively. Besides, there exists no correlation between δY and δCe, suggesting that the phosphorite was subjected to quite strong weathering and leaching processes, and catagenesis do not greatly modify its REE compositions.     

因柔至刚——宁海县图书馆设计札记

阅读是一种对话,一种参与,一种设身处地进入作者写作情境的旅程。该文结合宁海县图书馆设计分析阐述了通过建筑语汇表达更多的文化意味,柔性的院落空间烘托刚性建筑实体,概显建筑刚方正气的设计思路,在围合与开放之间的对比中造成内部空间深远的意味。图书馆设计应在空间与建筑上创造更多的人与环境、人与建筑之间的交流。使读者深入其中的过程成为精神旅程中的一次探索。     

江西省兴国县土壤侵蚀动态演变趋势分析

利用1958、1975、1982、2000年4期的土壤侵蚀强度等级图,空间配准及矢量化后,制成栅格分类图。在IDRISI 的CROSSTAB模块下分别计算了1958年到1975年,1975年到1982年及1982年到2000年的土壤侵蚀等级转换矩阵。根据该矩阵对兴国县土壤侵蚀的情况分期地进行了定量分析。结果表明:在研究的时期内,兴国县的土壤侵蚀经历了三个主要过程:1958年到1975年的侵蚀加剧期,1975年到1982年的自然恢复期,1982年到2000年的全面恢复期。到2000年,强度侵蚀的面积明显减少,无明显侵蚀的面积已达到全县面积的74.7%,严重土壤侵蚀状况已基本得到了控制。