新亚欧大陆桥新疆段环境灾害的灰色拓扑预测

基于灰色系统理论中拓扑预测的理论方法 ,对新亚欧大陆桥新疆段环境灾害造成的受损长度进行了分析预测 .在对受损长度时序分布特征分析的基础上 ,给定一组阈值 ξi,并按不同的时间序列分别建立 GM(1.1)模型而得到模型群 .然后应用新亚欧大陆桥新疆段 38年(1959～1997年)的受损长度统计资料 ,对所建模型群进行了检验 ,并用此模型群对未来可能出现一定阈值范围内受损长度的年份进行了预测 .经检验 ,该模型群的原点误差范围为 0.090～6.520 ,精度范围为 72.658～ 97.134.结果表明 ,所建模型群精确度高 ,科学性较强 ,具有比较好的实用性 .     

The Natural Vegetation Responses to the Groundwater Change Resulting from Ecological Water Conveyances to the Lower Tarim River

This paper takes the ecological water conveyance project (EWCP) that transfers water from the Bosten Lake, to Daxihaizi Reservoir, and finally to the Taitema Lake as a case study to analyze the dynamic change of the groundwater depth, the vegetation responses to the elevation of the groundwater depth as well as the relationship between the groundwater depth and the natural vegetation. The results from many years’ monitoring in field indicate: (1) the groundwater depth has been elevating gradually with the increase in the times of watering and the elevation range has been expanding continuously in the lower reaches of Tarim River. Correspondingly, the natural vegetation has a favorable response to the elevation of the groundwater depth. The change of the natural vegetation has accordance with that of the groundwater depth. Such facts not only show that groundwater is a key factor to the growth of the native vegetation but also prove it is feasible that the degraded ecosystem can be restored and protected by the EWCP; (2) the results of analysis of the spatial-temporal response of the natural vegetation to watering reveals that the beneficial influence of the EWCP on the ecosystem in the lower Tarim River is a long-term process; (3) in terms of the function and structure of ecosystem after watering in the lower reaches of Tarim River, the EWCP does not still reach the goal of ecological restoration at a large spatial scale at present. Based on such monitoring results, some countermeasures and suggestions for the future restoration strategy are proposed so as to provide a theoretical basis for restoring and protecting the ecosystem in Tarim River, and meanwhile it can also provide some scientific references for implementing the similar ecological projects in other areas.     

低温等离子体催化氧化甲烷的实验研究

采用电容耦合等离子体和催化剂协同作用对干空气中的甲烷进行了氧化实验,并和没有放置催化剂时进行了对比,结果表明,放置催化剂后甲烷的分解效率明显提高,反应产物中CO2的选择性增加,副产物NO和NO2的浓度减少,反应所需的能耗降低.甲烷的最终氧化产物为CO、CO2和H2O.     

新疆叶尔羌河突发性洪水初步研究

叶尔羌河发源于昆仑山和喀喇昆仑山区,是新疆第三大河。近30年,每2—3年发生一次突发性洪水,给下游人民造成很大灾难。 本文阐述了该洪水的特性,时空分布、演进情势及峰量变化,加之分析气象资料、地质地貌条件,首次提出突发性洪水成因于冰川阻塞湖泄洪,其策源地位于克勒青河上游的克亚吉尔特索湖和特拉木坎力湖。随着冰川的衰退,阻塞湖将逐渐缩小。     

阿拉善沙漠高原降水化学特征与离子来源判别

为查明我国北方沙漠地区降水化学组成及来源,在阿拉善沙漠高原阿右旗气象站采集了2013—2015年的降水样品,测定了降水pH、EC（电导率）及主要离子当量浓度.结果表明:阿拉善沙漠阿右旗气象站降水pH和EC的范围分别为6.66~8.05和35~1 237 μS/cm;Ca2+、SO₄2-、Na+和Cl-为降水中的主要离子,其总和占总离子的85%以上.降水pH、EC和主要离子当量浓度是反映空气质量的基本参数,较高的降水pH反映出当地降水具有明显的碱性特征.与其他地区相比,该地区降水的EC和可溶性离子日均湿沉降通量也较高,且随月份有较大的变化,表明干旱沙漠粉尘对当地降水水化学的贡献较大.根据离子来源相对贡献的计算结果发现,降水中92.8%的SO₄2-和98%的NO₃-来自人为源,98.8%的Ca2+和88.7%的K+为陆地来源,55%的Mg2+为海洋源,24.8%的Na+来自矿物风化,极少部分Cl-为人为源.研究显示:除降水中的NH₄+外,其他主要离子之间的相关性表明各种成因物质在风力作用下同时进入了大气;基于[NH₄+]（NH₄+的当量浓度）与[K+]（K+的当量浓度）相关性分析,降水中的NH₄+来自生物质燃烧、肥料使用、动物粪便等.      

美国包装废物管理、回收体系及产生回收状况

包装废物既产生于工业生产过程，也产生于商业物质循环流过程，更产生于居民的日常生活，是一类广泛存在的废物和资源。通过大量的资料和数据全面分析了美国的包装废物管理、产生和回收体系的特点和发展趋势，其中的一些经验可以为我国包装废物的管理提供借鉴。     

新型低温CuO/AC脱硫剂制备——煅烧温度对脱硫活性的影响

首次将炭载型ＣｕＯ／ＡＣ用于烟气脱硫,在最经济的烟气脱硫温度窗口（１２０～２５０℃）显示出高的脱硫活性．考查了煅烧温度和煅烧后脱硫剂的预氧化对脱硫活性的影响,并对脱硫剂进行了ＴＰＤ和ＥＸＡＦＳ表征．结果表明：经２５０℃煅烧的ＣｕＯ／ＡＣ脱硫剂具有最高的脱硫活性．２００℃煅烧,前驱体Ｃｕ（ＮＯ₃）₂未完全分解;高于２５０℃煅烧,活性组分ＣｕＯ被载体Ｃ部分还原为金属Ｃｕ 微晶,从而发生烧结、聚集,以上均导致脱硫剂活性的下降．尽管不同温度煅烧的ＣｕＯ／ＡＣ表现出大的脱硫活性差异,但吸硫后均生成同一反应产物ＣｕＳＯ₄．２５０℃煅烧的ＣｕＯ／ＡＣ脱硫剂Ｃｕ 以ＣｕＯ和Ｃｕ₂Ｏ形态存在,其中的Ｃｕ₂Ｏ在２００℃很容易氧化成ＣｕＯ     

Progress, Challenges and Prospects of Eco-Hydrological Studies in the Tarim River Basin of Xinjiang, China

Eco-hydrological research in arid inland river basins has been a focus of geologists and ecologists as it is crucial for maintaining the sustainable development of socio-economy, particularly in ecologically vulnerable areas. Based on the research work carried out in the Tarim River basin of Xinjiang, northwestern China, this paper summarizes synthetically the climate change and associated responses of water resources in the mountainous area, land use and land cover in the oasis, and plants responding to environmental stresses in the desert area of the river basin. Research gaps, challenges, and future perspectives in the eco-hydrological studies of the Tarim River basin are also discussed.     

Restoration of the lower reaches of the Tarim River in China

The middle and lower reaches of the Tarim River are areas of rich biodiversity and natural resources in the inland arid region of China. However, the Tarim River and its associated wetlands have been severely damaged and fragmented during the past several decades. To restore the deteriorated ecosystem and preserve the endangered riverine vegetation along the Tarim River, a project for releasing water from upper dams to the lower reaches of the Tarim River was initiated by China’s government in 2000. Between 2000 and 2005, we monitored the responses of groundwater levels and vegetation to this mitigation along nine transects spaced at mean intervals of 45 km along the river from Daxihaizi Reservoir, the source of water conveyance, to the Lake Taitema, the mouth of the Tarim River. We found that average groundwater levels rose significantly from 8 to 4 m below ground surface. Species diversity did not change during the 5-year period, but the total vegetation coverage and canopy size of some species significantly increased. The endangered tree species, Populus euphratica, started to regenerate. Our results indicated that species diversity might recover very slowly, even if the trial water release program became a permanent river management practice. Management decisions about allocating limited water supplies among competing uses in arid regions will ultimately determine whether degraded river ecosystems, such as the Tarim River, can be restored.