挖掘文化元素,打造榆城特色——浅谈赣榆新城和安湖湿地公园规划设计

本文以赣榆新城和安湖湿地公园的规划设计为例,从"和安文化"、"赣榆八景"等赣榆地方历史文化元素和海洋文化元素进行论述,探讨历史文化元素和海洋文化元素与现代景观交融的规划设计方法,塑造具有文化认同感,又适应现代人们生活需要的空间环境。

Technical analysis on the emergency handling of Tangjiashan barrier lake

This paper gives a brief introduction to the emergency handling of Tangjiashan barrier lake.Some technologies for the application of geological and topographical data are summarized and the mechanism of formation of a barrier lake is analyzed.Based on the safety status evaluation,the dam breach flood point is calculated.The paper concludes with discussion of the practical effects of emergency handling scenarios and different drainage channel designs.

Resettlement's impact on the domestic economy in lake restoration: a case study of Poyang Lake region

The Chinese government started a take restoration project in Poyang Lake region 10 years ago, and the expost mOnitor of the migrants＇ livelihoods was limited, This paper compares the composition difference of domestic income and domestic consumption between migration and non-migration villages in Poyang Lake region. The results show that the migrants＇ domestic income has increased in the last 10 years, which originated from the tncreasing trend of active and extensive rural labor migration, while the resettlement has not influenced the domestic income significantly. The resettlement stimulates younger farmers to work.far away from home whose wages contribute nearly 80% of domestic income, The resettlement decreases their savings due to higher expenditure of daily life for those who work far away from home, and higher expenditure of food for those who stay at home, losing cultivated lands with irrigation system for vegetable. On the other hand. the increase of rural labor migration leads the migrants who stay at home to have access to more cultivated lands for rice and cotton, and the farmers also apply more fertilizer in the same cultivated land for more agriculture products. The resettlement makes most of migrants spend their savings on the improvement of their housing conditions due to not enough governmental financial support for new building. After the analysis, some factors that influence migrants＇ income and consumption are discussed. The paper may contritbute to the building of Poyang Lake Ecological Economic Zone.

Contribution of Rupa Lake for Sustainable Food Security and Local Climate Change

Rupa Lake is small advancing eutrophic lake covering about 115 ha of the Lekhnath Municipality in Kaski district of western Nepal. The environment around the lake has been improved over a period of 10 years. Conservation practices were initiated by communities including the Rupa Lake Restoration and Fishery Cooperative （RLRFC）. As a result, an abundance of non-timber Forest Products （NTFP） has increased considerably. At present, 49 NTFP are available in the lake basin. Some households （HH） i.e 10% has additional income from NTFP. It is an indirect source of food security for local people. They sell NTFP products to generate income. A few households have already started farming of NTFPs. Availability of fodder and fuel wood from community forest has significantly contributed to the livelihoods of people where as wild edible fruits and vegetables have become supplementary for food security. There is yearly food security for 57% of HH with 22% having surplus food. 5% of HH has food security for less than three months where as 19% HHs have food security for more than six months. However, livelihood and nutritional security have improved by fish farming in lake. This lake is most important for the local environment and also helps eco-tourism. The study found that 92% observed the climate change in the form of a rise in temperature （〉 70% HHs）; unpredictable rainfall （〉 75% HHs）; shifting rainfall （〉 60% HHs）; phonological changes （〉 50%）. It showed that the lake supports the restoration of natural water capacity, maintain local climate and sound environment by better natural resource management for an environment friendly ecosystem.

行业特色高校外语“3+”培养模式创新与实践——以西安某高校高起点班为例

文章在高校人才培养多元化的趋势和大学英语改革的新背景下,以西安某行业特色型高校为例,论述了高起点本科生英语培养方案、目标及课程设置。并通过社会调查和课堂教学实践构建了一个针对高水平本科生的外语培养及教学模式,试图解决目前理工科院校大学英语课程设置不合理及教学模式单一的现象,为当前的高校的外语教育和外语改革提供一定的借鉴和参考作用。

斗潭湖变身记

衢州人都爱夸信安湖壮美,而我独爱娇小的斗潭湖。因为我曾经上过的幼儿园和现在上的小学就坐落在它的两岸,所以对它倍感亲切。更重要的是,我见证了斗潭湖发生的翻天覆地的变化,它越来越美丽了。早晨,每当上学路过斗潭湖时,我总会情不自禁地逗留欣赏一会儿风景。它就像一个美丽小魔仙深深吸引着我。湖的南北两岸柳树婆娑,风一吹,它们发出阵阵的'沙沙'声,翩翩起舞.

Lower Triassic Smithian-Spathian Boundary at West Pingdingshan Section in Chaohu,Anhui Province

The West Pingdingshan Section in Chaohu, Anhui Province, has been extensively studied in recent years and become one of the classic Lower Triassic sequences well-clarified in multiple stratigraphies. Also it is an important section that defines the Smithian-Spathian (S-S) boundary within the Olenekian Stage. The S-S boundary strata at the section are restudied in high-resolution conodont biostratigraphy and carbon isotopes. The refined S-S boundary defined by the FAD of conodont Neospathodus pingdingshanensis is at 30 cm above the base of Bed 52, corresponding to a rapid diversification of conodonts. A sharp positive shift of δ13Ccarb curve co-occurs at the S-S boundary and it can be used as a key reference to define the boundary. The defined S-S boundary position and carbon isotopes curve can be well correlated globally.

Formation and influencing factors of carbonate source rock of the Lower Permian Chihsia Formation in Chaohu region, Anhui Province

Highly-mature carbonate source rock is essential to the exploration of oil and gas in southern China. In this study, the carbonate strata in the relatively well-developed Lower Permian Chihsia Formation (located in Chaohu, Lower Yangtze) were targeted, and the formation and influencing factors of source rock were discussed based on paleoenvironment reconstruction using comprehensive sedimentology, palynofacies, and organic geochemistry data. The results demonstrate that the Chihsia Formation is oxygen-deficient biogenic carbonate sediments, with marked variations in the organic and inorganic components, formed during a period of Permian transgression. The formation of source rock is the combined result of high bioproductivity and oxygen-deficient environment generated by transgression and oxygenation events which frequently occurred during transgression periods. Source rock was affected by self-dilution effects and diagenesis, causing its heterogeneous distribution in many intervals. Source rock is over 40 m thick, and can be identified based on its different organic, biological, and mineral composition characteristics. The carbonate rock appears to require no specific clay content in order to become a source rock. The combination of sedimentology, palynofacies, and organic geochemistry has provided an effective means for evaluating and predicting high-maturity carbonate source rock in the region.