1) Yanergou watershed
燕儿沟流域
1.
In order to expand the little scale successful pattern to larger areas, it is appropriate for a middle scale area to be instanced in Yanergou watershed.
为能将这种模式推广到更大的地域范围 ,以位于延安的燕儿沟中尺度流域为例 ,在较为系统地分析和总结该流域“九五”期间产业基础建设和大农业发展方面所取得的工作业绩的基础上 ,对燕儿沟流域进行了生态环境效益、经济效益和可持续发展性评价 ,结果表明生态适宜型农村经济发展模式在中尺度条件下是有效的和可行
2) Yangou catchment
燕沟流域
1.
Influence of Vegetation Types on Soil Organic C at Yangou Catchment in the Loess Hilly-gully Region;
以黄土丘陵沟壑区燕沟流域为基础,分析了主要植被类型的SOC,TSN变化及其分布特征。
3) Yangou watershed
燕沟流域
1.
Sediment sources analysis of the Yangou watershed under a certain rainstorm event in the Hilly-gully Region of Loess Plateau;
延安燕沟流域次降雨泥沙来源分析
2.
Based on field survey and laboratory analysis,by using multi-linear stepwise regression and geographic information system(GIS),the paper studied the spatial distribution of surface soil(0-20 cm),organic C density in the Yangou watershed of loess hilly-gully region and its relationships with land use,landform,and so on.
通过野外调查和室内分析,采用多元线性逐步回归和地理信息系统(GIS)相结合的方法,研究了黄土丘陵区燕沟流域表层(0~20 cm)土壤的有机碳密度、空间分布及其与土地利用类型和地形因子等的关系。
3.
According to the research on the natural and artificial communities by five indexes of species diversity in Yangou watershed, this article discussed the relationship between re-vegetation ways (natural restoration, artificial restoration, natural and artificial restoration) and species diversity.
在燕沟流域选取 5个物种多样性指数对其天然及人工群落物种多样性进行了研究,分析了植被恢复重建途径(自然恢复、人工恢复、自然和人工恢复 )与物种多样性的关系。
4) Yan er gully
燕儿沟
1.
Report on data of monitoring sediment in Yan er gully Based on these data,tendency of reducing sediment amounts have been temporary analyzed.
对燕儿沟综合治理试验示范区水文泥沙监测资料作一通报 ,并以获得的泥沙资料为基础 ,对燕儿沟流域的治理减沙及泥沙来源情况作了初步分析 ,结果表明 :燕儿沟流域年输沙量有明显的递减趋势 ,并提出了目前监测工作存在的一些问题 ,以便为专题组工作顺利进行提供科学依
5) Chaigou Watershed
柴沟流域
1.
Study on Diversity of Vegetation Species of Chaigou Watershed in Wuqi County;
吴旗柴沟流域植被物种多样性研究
6) Hegou watershed
河沟流域
1.
In the new sites of afforestation with narrow terrace at Shanshuigou gully of Hegou watershed in Xixian,fixed sample spots were designed.
本文对隰县试区河沟流域山水沟水平阶整地的新造林地,设置固定观测样点,分别不同坡度、坡向和坡位对0~50cm土层水分状况进行了测定,分析了晋西南残塬沟壑区半干旱区不同条件下的水分差异及其动态,找出了造林关键时期浅层土壤水分变化规律。
补充资料:燕铁木儿
元文宗图帖睦尔时权臣。钦察人,功臣土土哈之孙。怀宁王海山镇守称海,燕铁木儿备宿卫十余年。海山即位,是为元武宗,封燕铁木儿同知宣徽院事。泰定帝致和元年(1328),任佥书枢密院事,掌宿卫。同年七月,泰定帝卒于上都。时燕铁木儿留大都,谋立武宗子为帝。八月,发动兵变,捕泰定帝在大都的支持者,夺中书省、枢密院权,遣人至江陵迎武宗次子怀王图帖睦尔至京。九月,图帖睦尔即位,是为文宗;同时,左丞相倒剌沙在上都立泰定帝子阿剌吉八为帝,是为天顺帝。双方激战,倒剌沙兵败投降。燕铁木儿以拥立之功,封太平王,拜中书右丞相、知枢密院事,加答剌罕号。图帖睦尔让位于当时远在漠北的长兄周王和世。天历二年(1329)正月,和世即位于和林之北,是为明宗,并立图帖睦尔为皇太子。三月,燕铁木儿北上迎和世,加拜太师。八月,途经王忽察都(今河北张北)时,与图帖睦尔合谋,将和世毒死,图帖睦尔再次即位,燕铁木儿独秉大权,所获赏赐不计其数,生活极端腐朽。至顺三年(1332)文宗卒,遗命立明宗之子为帝。明宗次子懿璘质班即位,是为宁宗,在位五十三日死,燕铁木儿欲立文宗子燕帖古思,文宗后不允,遂立明宗长子妥欢贴睦尔,是为顺帝。燕铁木儿惧怕杀害明宗的阴谋败露,心情不安,不久病死。子唐其势继为中书左丞相,女伯牙吾氏为顺帝后,元统三年(1335)均被右丞相伯颜杀死。
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