中下游 在 地理 分类中 的翻译结果
本文关键词:明清时期汉水中下游干堤修防的组织、管理与纠纷,由笔耕文化传播整理发布。
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Based on it, this paper took the Middle and Lower Reaches Tarim River for example from 1759 to 1949, it studied the implementation of the policy by the collection, the reorganization and analysis literature record. If there had been influence of the policy to the environmental changes was discussed? 基于此,本文选择1759-1949年塔里木河中下游地区为研究区域,,通过收集、整理和分析历史文献中对该地区屯垦活动、自然环境状况的记录,研究屯垦政策在该地区的实施情况,并在此基础上分析以下问题:特定时期的屯垦政策对环境变化有没有影响? 短句来源 Sensation And Reality:The Description of the River Landscape of the Middle and Lower Reaches of Han River in the Poems and Articles of the Song Dynasty as Well Its Explanations 感受与事实之间——宋人诗文所记汉水中下游河流景观及其解释 短句来源 THE RELATIONSHIP BETWEEN DROUGHTS,FLOODS AND CLIMATIC CHANGES IN THE MIDDLE AND LOWER REACHES OF THE CHANGJIANG RIVER SINCE LAST 1 000 YEARS 近1000年长江中下游旱涝与气候变化关系 短句来源 A Study on the Historical Changes of the Middle and Lower Reaches of the Bahe River and the Corresponding Influence on the Environment 灞河中下游河道历史变迁及其环境影响 短句来源 In fact, there were 56 tea-growing prefectures in the Tang Dynasty, distributed mainly in the middle and lower reaches of the Huaihe River and the Yangtze River. 唐代共有产茶州府56个,主要分布于淮河流域及长江流域中下游地区。 短句来源 更多 A PRELIMINARY STUDY ON THE MIGRATIONS AND THEIR SOCIAL EFFECTS IN THE DISTRICT OF THE MIDDLE AND LOWER REACHES OF THE YELLOW RIVER DURING THE EARLY PERIOD OF THE MING DYNASTY 明朝前期黄河中下游地区的移民活动及其社会作用初探 短句来源 The Organization, Administration and Conflict in Building and Protecting the Main Dykes at the Middle-lower Reaches of Han River During Ming-Ch'ing Period 明清时期汉水中下游干堤修防的组织、管理与纠纷 短句来源 During Ming-Ch 'ing period, there was an evident space-time discrepancy on both of the personnel assignment administration and the means of accumulating funds in the profession of building and protecting to the main dykes at the middle-lower reaches of Han River. 明清时期汉水中下游汉江干堤的修防在组织与管理、资金来源与运用上皆存在明显的时空差异。 短句来源 Secondly, it introduced the natural environment of the study area, which is the research' foundation stations troops to open up wasteland and the environmental variation. 第二部分是塔里木河中下游地区的自然状况。 该部分主要介绍研究区的地理位置、光热资源以及地形、绿洲情况,这是开展屯垦与环境变化研究的基础。 短句来源 Since the main channel of Middle and Lower Yangtze Rivers swing bank-to-bank frequently, and the section of river mouth has extended for a considerable distance to the East China Sea, the length of the Yangtze River is about 6300 km. 由于长江中下游下流主泓经常摆动,入海口段已有相当延长,故长江全长约为6300公里。 短句来源 更多
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middle and lower reaches
The chemical composition of water in the upper reaches of Ob' is determined by mercury and complex ore shows; in the middle and lower reaches, by catchments of major tributaries: Tom, Chulym, and, particularly, Irtysh.
Geochronology and isotope geochemistry of the CU-AU Mineralization belt in the middle and lower reaches of the Yangtze River are
In this paper, the Chebyshev polynomials in irregular grids are used in the forecast of precipitation distribution over the middle and lower reaches of the Changjiang River.
St abilization of summer monsoon in middle and lower reaches of the Changjiang river and seasonal transition of East-Asian circu
Using data of 850 hPa pentadal meanθs e and composite wind fields in East China, characteristics of the mean circulation are examined with summer monsoon (SM) stabilized over the Changjiang middle and lower reaches (CMLR).
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Usually a river has several headwaters on its source, but how to define the main source of a river lacks a univerally accepted principle or criterion. Some rivers define their main sources according to their lengths, and others define their main sources according to the traditional habit of the people .Under normal conditions, the traditional habit of the people coincides with the general flow direction of the river course, that is, if we make a survey from the plan map of a river network it looks like a natural...
Usually a river has several headwaters on its source, but how to define the main source of a river lacks a univerally accepted principle or criterion. Some rivers define their main sources according to their lengths, and others define their main sources according to the traditional habit of the people .Under normal conditions, the traditional habit of the people coincides with the general flow direction of the river course, that is, if we make a survey from the plan map of a river network it looks like a natural extention of its way from lower reaches to upper reaches. However, the quantity of water in a river usually doesnot define the main source.The source region of the Yangtze River headwaters is situated in the hinterland of Qinghai - Xizang plateau, which is an unlraveled region, so thah a consensus of opinions about where the main source of the Yangtze River rises is not yet attained .After thorough investigation, among the various headwaters of the Yangtze River, the Tuotuohe River is the longest (including the glacier on headwaters) by length, and the Dangqu River is slightly shorter. As to the criterion of unanimous direction of streams, Garqu River is the smoothest, and the Tuotuohe River next; by the discharge of water, Dangqu River ranks the biggest and Tuotuohe River the second gumming up the above considerations, the Tuotuohe River is both the longest and with approximately the same direction of streams.For this reason, we consider that the Tuotuohe River should be the main source of the Yangtze River.In accordance with the above standpoints, We have computed the length of the rivev section from the headwaters of the Tuotuohe River to Yibin of Sichuan province to be 3174 km; and the length of that section from Yibin to the river mouth about 2806 km.Since the main channel of Middle and Lower Yangtze Rivers swing bank-to-bank frequently, and the section of river mouth has extended for a considerable distance to the East China Sea, the length of the Yangtze River is about 6300 km.
江源水系诸河,地处青藏高原腹地,因人迹罕至,对那条河是长江正源,历史上并没有一个统一的认识可以遵循。通过考察后,在江源诸河中,论长度,沱沱河(包括源头冰川)最长,当曲稍次;论河道上下游的一致性,尕尔曲最顺,沱沱河其次;而论水量,当曲最丰,沱沱河其次。综合以上因素,我们认为沱沱河长度既长,方向又顺,应为长江正源。 综合上述观点,我们算得:由沱沱河源至四川省宜宾,长3474公里;宜宾至长江口约为2806公里。由于长江中下游下流主泓经常摆动,入海口段已有相当延长,故长江全长约为6300公里。
During the years of Hong Wu and Yongle in the Ming Dynasty, there appeared several largescaled, organized migrations along the middle and lower reaches of the Yellow River. This article discusses the social background of them, the process and the social functions of such migrations. It focuses on the following points.Each migration in the early years of Ming Dynasty is the result of one of the measures taken by the rulers to prevent the economy depressed by war from decline. The removal of the country's political...
During the years of Hong Wu and Yongle in the Ming Dynasty, there appeared several largescaled, organized migrations along the middle and lower reaches of the Yellow River. This article discusses the social background of them, the process and the social functions of such migrations. It focuses on the following points.Each migration in the early years of Ming Dynasty is the result of one of the measures taken by the rulers to prevent the economy depressed by war from decline. The removal of the country's political center (i.e. the removal of capital from Nanjing to Beijing) greatly diverts the migrations. Such changes stabilized the society then, quickeming the step of the economic blooming and flurishing, and developing the cultural intercourse among the people of the several provinces along the middle and lower reaches of the Yellow River. Especially the large scaled migrations from the area around Shanxi province into Beijing greatly balanced the population, and solidified Beijing's position in politics, economy and military superiority.
明朝洪武、永乐年间,黄河中下游地区发生过多次有组织的大规模人口迁移活动。本文初步探讨了它们的社会背景、迁移过程及其在不同时期的特点,论述了人口迁移在稳定社会局势、恢复农业经济、促进文化交流等方面的作用。
This article approaches to the origin of the silkworm and silk-knit industry in China.From some traditions on historical records, and some archaeological finds, it is proved that the original place of the silkworm and silk-knit in dustry was not only one, but multicentres and multiorigins. Original places were mainly distributed in the regions along the lower reaches of the Changjiang River and the middle and lowerr eaches of the Huanghe Rive.They originated from the Huangdi age in the Neolithic age about 5000...
This article approaches to the origin of the silkworm and silk-knit industry in China.From some traditions on historical records, and some archaeological finds, it is proved that the original place of the silkworm and silk-knit in dustry was not only one, but multicentres and multiorigins. Original places were mainly distributed in the regions along the lower reaches of the Changjiang River and the middle and lowerr eaches of the Huanghe Rive.They originated from the Huangdi age in the Neolithic age about 5000 years B.P.. By analysing the geographical conditions in the lower reaches of the Changjiang River and the middle and lower reaches of the Huanghe River, it is not accidental that the silkworm and silk-knit industry originated there.
本文根据历史传说、古籍记载、考古发掘,阐述我国蚕丝织业的起源是多中心多源头的,并从蚕、桑生长的适宜生态环境分析,说明黄河中下游及长江下游地区为蚕桑丝织业发源地的合理性。
 
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本文关键词:明清时期汉水中下游干堤修防的组织、管理与纠纷,由笔耕文化传播整理发布。
本文编号:157911
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