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Халдвар тархах үйл явц: нийгэм-сэтгэл зүйн болон социаль үндэс “2012.12.21”- ны жишээн дээр
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Ядуурлын учир шалтгаанд хийсэн дүн шинжилгээ
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Монголчуудын бие биенээ дэмжин туслах уламжлалт харилцааны тухай асуудалд
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Хүүхдийн нийгмийн оролцоог дэмжих асуудалд
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ЭРХ ЗҮЙН СОЦИОЛОГИЙН ИНТЕГРАТИВ ШИНЖ: ЭРХ ЗҮЙН СОЦИОЛОГИЙН ИНТЕГРАТИВ ШИНЖ
No full textAbstract: The sociology of law (or legal sociology) is often described as a sub-discipline of sociology or an interdisciplinary approach within legal studies. Some see sociology of law as belonging "necessarily" to the field of sociology whilst others tend to consider it a field of research caught up between the disciplines of law and sociology. Still others regard it neither as a sub-discipline of sociology nor as a branch of legal studies but as a field of research on its own right within the broader social science tradition. Accordingly, it may be described without reference to mainstream sociology as "the systematic, theoretically grounded, empirical study of law as a set of social practices or as an aspect or field of social experience",. It has been seen as treating law and justice as fundamental institutions of the basic structure of society mediating "between political and economic interests, between culture and the normative order of society, establishing and maintaining interdependence, and constituting themselves as sources of consensus, coercion and social control". Irrespective of whether sociology of law is defined as a sub-discipline of sociology, an approach within legal studies, or a field of research in its own right, it remains intellectually dependent mainly on the traditions, methods and theories of mainstream sociology and, to a lesser extent on other social sciences such as social anthropology, political science, social policy, criminology and psychology; as such, it reflects social theories and employs social scientific methods to study law, legal institutions and legal behavior.
More specifically, sociology of law consists of various approaches to the study of law in society, which empirically examine and theorize the interaction between law, legal, non-legal institutions and social factors. Areas of socio-legal inquiry include the social development of legal institutions, forms of social control, legal regulation, the interaction between legal cultures, the social construction of legal issues, legal profession, and the relation between law and social change.
Sociology of law also benefits from and occasionally draws on research conducted within other fields such as comparative law, critical legal studies, jurisprudence, legal theory, law and economics and law and literature
ЭМЭГТЭЙЧҮҮДИЙГ УЛС ТӨРИЙН ШИЙДВЭР ГАРГАХ ТҮВШИНД ХҮЛЭЭН ЗӨВШӨӨРӨХ ИРГЭДИЙН ХАНДЛАГА
No full textAbstract: Mongolian female political representation of women in decision-making by 2013 , 30 % lead to achieving the Millennium Development Goals .Increase women ‘s political participation and decision -making selection of voters , it is important to consider the situation . Thus, citizens’ attitudes in female politiciansand to determine ways to increase the number of women in political decision - making , this article will present a summary of research conducted between 2012-2013
СУРГУУЛИЙН ӨМНӨХ НАСНЫ ХҮҮХДИЙН ЭРҮҮЛ МЭНДЭЭ ХАМГААЛУУЛАХ ЭРХИЙН ЗАРИМ АСУУДАЛ
No full textAbstract: Recent years Mongolia has some positive factors, which is increase of birthrate, rise of population, but it has some negative sides also. For example: lack of kindergarten, safety and hygiene,right to public health service, right to study(lack of efficient, creative and well-educate ,humanitaryaproach to work with new century children). Aimed to concentrate one’s attention on a problem like pre-school education health care and other rights been irritated
Significance Articles of Education in Constitutional Framework - Through a comparison of the Constitution of Japan and the Constitution of the Empire of Japan -
No full textThis thesis examines the articles related to education in two types of constitutions in Japan. The history of modern constitution in Japan dates back to 1889, 135 years ago. The Constitution of the Empire of Japan established in 1889 for building the constitutional regime and respond to pressures from the Western powers, known as “The Meiji Constitution” after the name of the era at that time, was the Constitution granted by the Emperor. The Meiji Constitution inherited the Prussian Constitution (1848/1850) that contained many articles on education, but The Meiji Constitution itself did not contain any articles on education. Conversely, the current Constitution of Japan established in 1946 which is formally revised of The Meiji Constitution has multiple provisions regarding education, but the Constitution of the United States, on which it is based, has no provisions on education due to its federal structure. Of course, these differences arise from the social or political backgrounds, particularly legal inheritances to each constitution. Therefore, in this thesis, to explore the following points: (1) despite having inherited the Prussian Constitution, the reasons why there were no articles on education in The Meiji Constitution and how educational activities were carried out under those circumstances, (2) the features of the provisions about education in the current Constitution and the educational system based on them, and (3) the significance of positioning education in the Constitution through a comparison of the two, additionally, clarifying the differences of the meaning between articles of education under the Imperial Constitution and those under the Democratic Constitution, and examine the pros and cons of constitutional control over education.
Үндсэн хуулийн тогтолцоо дахь боловсролын тухай заалтуудын ач холбогдол - Японы Үндсэн хууль болон Японы эзэнт гүрний Үндсэн хуулийн харьцуулсан судалгаа -
 
Climatic Study of Site of Chinggis Khaan International Airport in the Khushig Valley: Хөшигийн хөндийд байрлах Чингис хаан олон улсын нисэх онгоцны буудал орчмын уур амьсгалын судалгаа
No full textIn connection with the construction of a new international airport, the Civil Aviation Administration of Mongolia made a decision to urgently develop a climate profile for the Khushig Valley in 2001. Within the framework of this decision, researcher B. Jigmeddorj developed a climate profile for the area in 2007. The climate profile was developed using data from the automatic weather station located in the Khushi Valley for the years 2002-2006. Although the climate profile developed by B. Jigmeddorj met the requirements of the time, it had shortcomings such as the lack of night-time meteorological observations and visual observations of weather phenomena. On the other hand, it is relatively outdated in terms of time and does not fully meet current requirements. Therefore, this study aimed to develop a climate profile for the Khushi Valley area using actual observation (METAR) data. During the study period, the average air temperature in the Khushi Valley area was -0.4°C, the absolute maximum temperature reached 34.0°C in July, and the absolute minimum temperature reached -39.0°C in January. The absolute minimum temperature reached -2.0°C in January, it reached 6.0°C in July, and it was below 0.0°C in the months other than the summer months, for example, -7.0°C in May and -10.0°C in September. The annual total precipitation in the Khushig Valley area was 249.7 mm. The frequency of no wind or “calm” is 23-41%, while the prevailing wind directions are from the Northwest (NW), West (W), East, northeast (ENE), and East (E). The highest frequency of strong winds mainly blows from the Northwest (NW) and North, northwest (NNW). The average wind speed of more than 4 m/s in any month or at any time of the day is considered to be a very windy area around the aerodrome in the Khushi Valley. Despite the high wind speed, the wind from the East, Southeast (ESE) and the West, Northwest (WNW), i.e. the tailwind frequency on the runway is low, namely, the wind speed above 16 m/s was observed only 4 times during the entire measurement period. Winds of 5 m/s and above along the runway are local or from the East (E), while winds of 12 m/s and above along the runway are crosswinds or from the West, Northwest (WNW). The number of cases where the base of the lower atmosphere was 300 m or lower was 0.07-0.11% of the total measurements between 22:00 and 02:00, 0.14-0.16% of the cases observed between 301 and 600 m, and 0.01% of the cases observed in the layer of 601 and 800 m. The study considered the number of cases of lower atmosphere clouds BKN - cloudy (5-7 octas), OVC - overcast (8 octas). It was found that the frequency of cases reaching the OVC level in the spring season near the aerodrome located in the Khushig Valley reaches almost 23.2%
Delineating the boundary between the Mongolian Altay and Gobi-Altay Mountain Ranges: A Geomorphic and Geographical Approach: Монгол Алтай, Говь-Алтайн нурууны хил заагийг тогтоох асуудалд: Газарзүй болон геоморфологийн хандлага
No full textThis study addresses the long-standing academic issue of delineating the boundary between the Mongolian Altay and Gobi-Altay mountain ranges in southwestern Mongolia. A combination of comparative geomorphological analysis and morphometric methods was employed. The results reveal that the Mongolian Altay is characterized by relatively high elevations, glaciated peaks, a more humid climate, widespread permafrost, well-developed altitudinal zonation, and distinctly differentiated landscapes. Geologically, it is dominated by Paleozoic metamorphic and intrusive rocks. Geomorphologically, erosional landforms prevail. In contrast, the Gobi-Altai range exhibits lower elevations, arid climate, limited permafrost distribution, weak altitudinal zonation, and less pronounced landscape differentiation. Its geological structure is characterized mainly by relatively young sedimentary and intrusive rocks, while geomorphologically, both depositional and erosional landforms are common. A key outcome of the present study is the identification of the Huvch - Alag Lake fault zone - extending approximately 100 km - as a morphostructural boundary between the two mountain systems. Morphometric indicators such as hypsometric integral (HI > 0.71), mountain front sinuosity (MFs ≈ 1.1), and steep fault-related slope angles (RSl > 65-71°) provide strong evidence of tectonic and morphostructural contrasts along this fault zone. Furthermore, differences in landscape structure, climate, vegetation, and permafrost distribution reinforce the validity of this boundary. These findings contribute to a more precise classification of Mongolia’s mountain systems and offer significant insights into the ongoing geodynamic processes driven by the India–Eurasia continental collision. Additionally, the study provides a scientific basis for regional ecological, tectonic, landscape, and geomorphological regionalization, as well as for the assessment and sustainable use of natural conditions and resources