稻城亚丁的旅游环境承载力分析

旅游环境承载力是有一定限度的,尤其是像稻城亚丁这样生态环境脆弱的地域,生态环境一旦遭到破坏就难以恢复,客观上必然要求在进行旅游资源开发规划设计时对旅游开发强度及其可能引起的环境负荷做慎重考虑.在对稻城亚丁旅游资源进行介绍的基础上,运用科学的方法从环境生态承载量、资源空间承载量、心理承载量和经济承载量对其旅游环境承载量进行测量,针对测算结果提出相应的建议.     

石油降解固态菌剂的研制

用喷雾干燥和表面吸附固定化两种工艺对石油降解菌剂进行固态菌研制。结果表明:在对菌浓度为9.7×109 cfu/mL的500mL发酵液添加40g轻质碳酸钠后进行喷雾干燥,在进风温度为120℃,进样量为12mL/min的条件下,得到粉剂产品56g,含水量为4.6%,菌密度为10.05×109 cfu/g,产品得率为11.6%;在对菌浓度为9.7×109 cfu/mL的500mL发酵液添加1 500g麸皮进行吸附固定化处理,得到粉剂产品1 438.6g,水分含量为7.9%,菌密度为5.7×108 cfu/g,产品得率为16.9%。考虑到喷雾工艺设备投资大,能耗多等不利因素,因此建议使用吸附固定化技术作为石油降解固态菌剂的下游处理技术。     

稠油污泥资源化处理技术研究进展

石油开采和加工过程会产生大量的含油污泥,其成分复杂、稳定性高、处理难度大,已成为影响石油生产的主要污染因素,因此寻找出合理的含油污泥资源化处理技术十分必要。文章综述了稠油污泥的处理方法和不同油田针对其污泥采用的工艺流程,着重介绍了热解处理的原理和试验方法,并且对含油污泥处理技术未来的发展方向做出展望。     

河南鸡冠洞洞穴水对极端气候的响应及其控制因素研究

为揭示洞穴水地球化学动态的变化特征及其控制因素,从2009年10月至2013年12月对黄土高原东南缘河南西部栾川县鸡冠洞洞穴水的水化学指标进行了4个完整水文年的动态监测.结果表明:1鸡冠洞洞穴水的化学类型主要是HCO-3-Ca2+-Mg2+和HCO-3-Mg2+-Ca2+型,阴离子中HCO-3占80%以上,阳离子中Ca2+、Mg2+是优势离子,地下河常年处于溶蚀状态,池水、滴水处于沉积状态.2鸡冠洞洞穴滴水、池水可以很好地响应外部气候环境的变化,其地球化学指标具有显著的季节效应.3Ca2+、Mg2+、SO2-4能够敏感地响应极端气候事件引起的年际降水量变化,Ca2+、Mg2+、SO2-4浓度洪涝年升高,干旱年降低.HCO-3主要受CO2浓度控制,对极端气候事件响应不明显.4鸡冠洞地下河中Ca2+、Mg2+、HCO-3、SO2-4浓度波动幅度较小,且无明显的季节变化规律.对2010年和2013年的极端降水事件响应不明显.     

Predicting Nitrogen Loading With Land-Cover Composition: How Can Watershed Size Affect Model Performance?

Watershed-wide land-cover proportions can be used to predict the in-stream non–point source pollutant loadings through regression modeling. However, the model performance can vary greatly across different study sites and among various watersheds. Existing literature has shown that this type of regression modeling tends to perform better for large watersheds than for small ones, and that such a performance variation has been largely linked with different interwatershed landscape heterogeneity levels. The purpose of this study is to further examine the previously mentioned empirical observation based on a set of watersheds in the northern part of Georgia (USA) to explore the underlying causes of the variation in model performance. Through the combined use of the neutral landscape modeling approach and a spatially explicit nutrient loading model, we tested whether the regression model performance variation over the watershed groups ranging in size is due to the different watershed landscape heterogeneity levels. We adopted three neutral landscape modeling criteria that were tied with different similarity levels in watershed landscape properties and used the nutrient loading model to estimate the nitrogen loads for these neutral watersheds. Then we compared the regression model performance for the real and neutral landscape scenarios, respectively. We found that watershed size can affect the regression model performance both directly and indirectly. Along with the indirect effect through interwatershed heterogeneity, watershed size can directly affect the model performance over the watersheds varying in size. We also found that the regression model performance can be more significantly affected by other physiographic properties shaping nitrogen delivery effectiveness than the watershed land-cover heterogeneity. This study contrasts with many existing studies because it goes beyond hypothesis formulation based on empirical observations and into hypothesis testing to explore the fundamental mechanism.     

监控完全遮挡场景下火焰特征分析方法*

为解决监控完全遮挡场景下火灾原因认定面临的问题,探究火焰的视频特征分析方法。利用油盘火、垃圾桶火焰和短路火花3种实体火焰模拟室内火灾,布置普通彩色CCD监控摄像头使之被完全遮挡,收集火灾视频进行预处理,利用视频分析技术提取、对比、分析油盘火焰、垃圾桶火焰和短路火花的HSV颜色、火焰面积增长、质心变化、Harris角点变化、火焰频闪等特征,并总结对应特征变化规律。结果表明:在监控完全遮挡场景下,提出的火焰视频特征分析方法可以较为精确地定量表征火焰动静态特征,为火灾调查工作的顺利开展提供有力的工具。     

气-固耦合作用下煤层气注热开采热量迁移规律数值模拟

为获取气固耦合作用下煤层气注热开采过程热量分布规律,探究煤层内气-固体系吸热量的影响因素,采用自行研制的三轴煤层气解吸热量测试验装置,在实验室中对柱状原煤进行了不同轴、围压条件下煤体甲烷解吸过程温度及热量变化测定,利用温度补偿原理获取了解吸热与解吸量关系理论模型,利用COMSOL Multiphysics软件进行了煤层气注热开采过程热量迁移规律数值模拟.结果表明:解吸热随解吸量呈指数增长趋势;模拟结果显示井间距为60 m时相较于40 m时煤层吸热量更快达到稳定,吸附气体吸热量升高持续时间为井间距40 m时的1.9倍;解吸热量在注热温度为593 K时较注热温度为493 K时增加15.97％,且达到最终解吸热量稳定时间减少21.4％.对比分析得到,在单井注热开采条件下,增大井间距和提高注热温度均可以不同程度影响热量在煤层中迁移、增大解吸热量并促进解吸作用,进而大幅度提升煤层气井筒累计产量.研究结果可为低渗透储层煤层气高效安全开采及煤层气注热开采工艺方案优化提供理论支撑.     

Fe掺杂Bi2MoO6的制备及其可见光催化活化PMS降解橙黄Ⅱ的研究

采用一锅水热合成法制备Fe掺杂Bi2MoO6光催化剂,对Bi2MoO6的主体结构进行修饰和调整.在可见光LED照射下,利用合成的Fe-Bi2MoO6催化剂活化过一硫酸盐(PMS,peroxymonosulfate,oxone)对偶氮染料橙黄Ⅱ进行光催化降解.采用X射线衍射(XRD),扫描电子显微镜(SEM),透射电子显微镜(TEM),X射线能谱(XPS)和紫外-可见漫反射光谱(UV-Vis)对催化剂的形貌微观结构和化学价态进行表征,并应用在光催化活化PMS降解橙黄Ⅱ的过程中.结果表明,催化剂投加量为0.4 g/L,PMS投加量为0.4 mmoL/L,初始pH值接近中性条件下,Fe-Bi2MoO6材料对橙黄Ⅱ的去除率可以达到100％.经过Fe掺杂后,Fe取代一部分的Bi3+,致使主体晶格出现畸变,不仅有利于光生电子和空穴的产生、分离和转移,还增强了 Bi2MoO6的光催化活性.Fe-Bi2MoO6光催化剂经重复使用5次后对橙黄Ⅱ的降解率仍然可以达到89.1％以上,具有优秀的光催化稳定性能.活性自由基的出现在光催化降解过程中起到主要作用,由此展示出一种潜在的光催化降解机制,且Fe掺杂Bi2MoO6比单纯Bi2MoO6具有更好的光催化降解稳定性.     

臭氧催化氧化控制溴酸盐生成效能与机理

比较了单独臭氧氧化和金属氧化物存在下臭氧催化氧化过程中溴酸盐的生成规律,探讨了催化剂投量、溴离子浓度、水的pH值、反应温度等对臭氧催化氧化控制溴酸盐生成的影响规律及在催化剂存在下控制溴酸盐生成的机理.结果表明,催化剂投量从0 mg/L增加到250 mg/L,能减少溴酸盐生成量85.1%;当溴离子浓度为0.5、1.0、2.0 mg/L时,臭氧催化氧化分别能减少溴酸盐生成量69.2%、83.5%和15.2%,溴离子浓度变化对催化作用的影响无明显规律;pH值升高会降低催化作用的效果;反应温度在5～25℃之间时,臭氧催化氧化能降低43%～59%的溴酸根生成量(溴离子浓度1.5 mg/L),反应温度变化不影响催化效果.催化剂通过抑制臭氧对次溴酸的氧化减少了溴酸根的生成量.催化剂表面的某些基团与硫酸根络合会削弱臭氧催化氧化控制溴酸根生成的能力,因此,利用催化剂控制溴酸盐的机理与催化剂表面性质密切相关.     

Middle-Eocene artiodactyls from Shanghuang (Jiangsu Province,Coastal China) and the diversity of basal dichobunoids in Asia

A new assemblage of basal dichobunoid artiodactyls from the middle-Eocene Shanghuang fissure fillings includes the diacodexeid Jiangsudon shanghuangensis gen. and sp. nov., a new species of the lantianine dichobunoid Elaschitotherium, Elaschitotherium crepaturus sp. nov., and an indeterminate suoid which is presently the earliest record of this clade. Diacodexeids are also represented by two forms provisionally referred to cf. Diacodexis sp. and to an indeterminate Diacodexeidae, respectively. The occurrence of diacodexeids in Shanghuang contrasts with the early and earliest middle-Eocene chronological range of the family in Europe and North America and suggests that the stratigraphic range of the family in Asia extends up to the middle Eocene. This may reflect particular habitats in coastal China that may have been relatively stable during the early and middle Eocene, thus preserving forest-dwelling artiodactyls that became extinct in the other Holarctic regions. Compared to other supposedly coeval North American, European, and Asian faunas, the Shanghuang mammalian assemblage is most similar to early Uintan faunas of North America but is also remarkable in recording forms close to taxa that are characteristic of the Wasatchian and Bridgerian North American Land Mammal Ages. The Irdinmanhan age of the Shanghuang fauna is supported by the mammalian assemblage recovered from the fissure D, but an Arshantan age cannot be completely ruled out at this point. Although the Shanghuang assemblage is biased towards preservation of small components of the mammalian fauna, the Shanghuang fauna provide an important and unique window into the Eocene diversity and early evolution of cetartiodactyls in eastern Asia.