内蒙古食盐产地分布和变迁研究
发布时间：2019-02-14 09:36
【摘要】：目前学术界对内蒙古地区食盐产地方面的研究还相当薄弱,至今尚无专文和专著。本文在对所搜集的材料进行认真分析的基础上,将内蒙古地区出现过的和现存的食盐产地的变化情况梳理清楚。同时,考证出了许多前人不曾研究或注意到的产地,为现今盐业资源的开发和有效利用提供借鉴。 内蒙古地区食盐产地众多,分布广泛,以池盐和土盐为主,池盐为大宗。鄂尔多斯、阿拉善和锡林郭勒盟产地较多,其他地区较少。鄂尔多斯有盐池32处,其中已废弃11处。阿拉善地区有盐池26处,以吉兰泰盐池和雅布赖盐池为最大,其他规模较小,除吉兰泰和雅布赖等几个较大的盐池依旧在进行食盐生产外,其他皆已废弃。锡林郭勒盟计有食盐产地17处,其中池盐产地16处,土盐产地1处,以产青盐和白盐著称。巴彦淖尔市、呼和浩特市、包头市、乌兰察布盟食盐产地较少,且较分散,计有池盐产地9处,土盐产地11处。赤峰市、兴安盟和呼伦贝尔盟池盐产地较少,且较分散,开发利用较晚,计有11处;土盐产地不定,存在时间较短,皆已不在进行食盐生产。 就食盐产地分布而言,池盐产地在整个内蒙古地区皆有分布,其中以鄂尔多斯、阿拉善和锡林郭勒盟较多,其他地区次之。土盐产地分布相对集中,主要分布于呼和浩特、包头、乌兰察布盟一带和锡林郭勒盟西南部。本文按照地域论述食盐产地分布及变迁,尽可能把每个地区自古至今所有的食盐产地都找出来,把每个产地的有关情况都搞清楚。
[Abstract]:At present, the research on the origin of salt in Inner Mongolia is still relatively weak, and there are no special papers and monographs to date. On the basis of careful analysis of the collected materials, this paper makes clear the changes of the origin of salt in Inner Mongolia. At the same time, it is proved that many places have not studied or noticed, and provide reference for the development and effective utilization of the current salt industry resources. The salt in Inner Mongolia has a large number of salt and is widely distributed. It is mainly composed of the salt and the soil salt, and the salt of the pool is large. Zong. Erdos, Alashan and Xilingguo are more in production, and the other areas are more. Less. There is a salt pool 32 in Erdos, where 11 is discarded. The salt pool 26 of the Alashan area is the largest and the other smaller, except that several large salt tanks, such as Gillantai and Jaibriai, are still in salt production, and the others have been used. The site of salt production is 17 at the site of salt, where the salt of the salt is 16, and the salt of the earth is 1, to produce the salt and the white salt. It is said that the salt production area of the city of Bayannul, Hohhot, Baotou and Ulaanqabu is less, and is more dispersed, with the salt producing area of 9 and the origin of the soil salt 11. At the same time, the origin of salt in Chifeng, Xingang and Hulunbele is relatively small, and the development and utilization of the salt are relatively late, with 11 places; the place of the soil salt is indefinite, the time is short, and no salt is present in that case of the distribution of the origin of the table salt, the origin of the pool salt is distribute throughout the whole of the Inner Mongolia area, including the Ordos, Alashan and the Xilingol League, and the other place The area is the second place. The distribution of soil salt is relatively centralized, mainly distributed in Hohhot, Baotou, Ulaanqabu and Xilingol League. in that south-western part of the region, the distribution and the change of the origin of the table salt are discus in terms of geographical area.
【学位授予单位】：湘潭大学
【学位级别】：硕士
【学位授予年份】：2011
【分类号】：K249
本文编号：2422086
[Abstract]:At present, the research on the origin of salt in Inner Mongolia is still relatively weak, and there are no special papers and monographs to date. On the basis of careful analysis of the collected materials, this paper makes clear the changes of the origin of salt in Inner Mongolia. At the same time, it is proved that many places have not studied or noticed, and provide reference for the development and effective utilization of the current salt industry resources. The salt in Inner Mongolia has a large number of salt and is widely distributed. It is mainly composed of the salt and the soil salt, and the salt of the pool is large. Zong. Erdos, Alashan and Xilingguo are more in production, and the other areas are more. Less. There is a salt pool 32 in Erdos, where 11 is discarded. The salt pool 26 of the Alashan area is the largest and the other smaller, except that several large salt tanks, such as Gillantai and Jaibriai, are still in salt production, and the others have been used. The site of salt production is 17 at the site of salt, where the salt of the salt is 16, and the salt of the earth is 1, to produce the salt and the white salt. It is said that the salt production area of the city of Bayannul, Hohhot, Baotou and Ulaanqabu is less, and is more dispersed, with the salt producing area of 9 and the origin of the soil salt 11. At the same time, the origin of salt in Chifeng, Xingang and Hulunbele is relatively small, and the development and utilization of the salt are relatively late, with 11 places; the place of the soil salt is indefinite, the time is short, and no salt is present in that case of the distribution of the origin of the table salt, the origin of the pool salt is distribute throughout the whole of the Inner Mongolia area, including the Ordos, Alashan and the Xilingol League, and the other place The area is the second place. The distribution of soil salt is relatively centralized, mainly distributed in Hohhot, Baotou, Ulaanqabu and Xilingol League. in that south-western part of the region, the distribution and the change of the origin of the table salt are discus in terms of geographical area.
【学位授予单位】：湘潭大学
【学位级别】：硕士
【学位授予年份】：2011
【分类号】：K249
【参考文献】
相关期刊论文 前7条
1 郭正忠;西夏地区古盐产资源考辨——兼论若干宁甘古盐池的位置[J];宁夏社会科学;1993年06期
2 王冠倬;;从一行测量北极高看唐代的大小尺[J];文物;1964年06期
3 吉成名;;论影响食盐产地变化的因素[J];湘潭大学学报(哲学社会科学版);2010年02期
4 吉成名;;西夏食盐产地研究[J];盐业史研究;2006年01期
5 吉成名;;论金代食盐产地[J];盐业史研究;2008年03期
6 王乃昂;何彤慧;黄银洲;冯文勇;程弘毅;;六胡州古城址的发现及其环境意义[J];中国历史地理论丛;2006年03期
7 吉成名;;元代食盐产地研究[J];四川理工学院学报(社会科学版);2008年03期
相关会议论文 前1条
1 吉成名;;汉代食盐产地研究[A];盐文化研究论丛(第二辑)[C];2007年
相关博士学位论文 前1条
1 李青淼;唐代盐业地理[D];北京大学;2008年
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