1) Yili River
伊犁河
1.
The Native Fisher Distributed and Made of Evolution in the Yili River (China s Section);
伊犁河(中国境内)土著鱼类的分布与演化
2.
Primary Survey on Summer Birds in Yili River Wetland and Its Vicinity
新疆伊犁河湿地及周边夏季鸟类调查初报
3.
The survey of water quality on Tekes River and Yili River in xinjiang was carried out from August 2004 to August 2006.
通过2004—2006年对伊犁地区的特克斯河、伊犁河的水质调查及水质标识指数和综合指数(WQI)的计算发现,DO、COD、TN、NH3-N、TP 5项指标在10个断面的空间分布上伊宁市区的2个断面水质最差,在时间上属8月最差,水质主要污染指标的排序依次为TP、TN、COD和NH3-N。
2) The Yili River
伊犁河
1.
Consideration on water-saving irrigation in the Yili River basin;
伊犁河流域节水灌溉的思考
3) Yili River Valley
伊犁河谷
1.
Environmental Analysis and Comprehensive Evaluation of Ecotourism Resources in Yili River Valley;
伊犁河谷生态旅游资源环境分析及评价
2.
On Identity of Eco-tourism and Product Design in Yili River Valley;
伊犁河谷生态旅游形象定位及产品设计
3.
In the last few years,the tourism development is quite rapid in Yili river valley,but tourism development gets behind with others areas by a long way.
近年来伊犁河谷旅游业虽取得了很大的发展,但与相邻地区相比,差距明显,文章拟通过对伊犁河谷旅游资源的概念性评价和旅游资源整合条件分析,提出旅游整合开发的思路构想,为区域旅游业竞争力的提升和经济一体化的实现有所裨益。
4) By the Side of the Yili River
伊犁河畔
5) Yili Valley
伊犁河谷
1.
Extreme Weather and Climate Change over Yili Valley in Spring and Summer
伊犁河谷春夏季极端天气气候的变化分析
2.
Study on the tourism production exploitation in Yili Valley of Xinjiang
新疆伊犁河谷地区旅游产品开发的战略研究
3.
Yili Valley of Xinjiang was taken as a sample to sort out regional tourism resources classification.
文中以新疆伊犁河谷地区为案例,梳理区域旅游资源类型,在此基础上分析了竞争型旅游资源类型和旅游资源市场竞争力,并以竞争型资源为主要吸引物提出旅游资源的空间区域整合开发方案。
6) Ili River valley
伊犁河谷
1.
Investigation and Analysis on Cold Damage of Apple in Ili River Valley
伊犁河谷苹果冻害调查分析
2.
Investigation on Legume Plants Resources in the Ili River Valley
伊犁河谷地区豆科植物资源的初步研究
3.
The erosion traits of melted- snow were studied during spring from March 3 to March 10,2009,at Ili River valley slope land.
采用坡面径流小区试验法,于2009年3月3～10日,对伊犁河谷缓坡地的春季融雪侵蚀特征进行了系统研究。
补充资料：伊犁河
| 伊犁河 位于天山山脉西段。上游在中国新疆维吾尔自治区西部。长约440千米，流域面积5.5万平方千米。上游有三源：特克斯河、巩乃斯河、喀什河。特克斯河是主源，出汗腾格里峰北坡，东流与巩乃斯河汇合后称伊犁河。西流至雅马渡有喀什河流入。以下进入宽阔的河谷平原，河床宽大，支汊和沙洲众多，下游在接纳了支流霍尔果斯河后流入哈萨克斯坦，最后注入巴尔喀什湖。河水由冰雪融水和雨水补给。春汛连结夏汛，汛期长，径流量年际变化较小，有利于农业灌溉。干流下游每年5～10月可通航船只。
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参考词条