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At the beginning of the 1950s, the nationality policy of the People's Republic of China granted the Sui, a Tai-speaking minority (Kam-sui group of the Kadai branch) in southern Guizhou, the status of nationality under the Chinese name "shui" and allocated them an autonomous administrative territory in their name with the rank of district. The study presented here provides an example of the territorial production of the Chinese state captured on a local scale, where questions of ethnic identification and regional autonomy present their own configurations. We begin by examining the classification procedures of the Qing imperial state, which at the end of the seventeenth century drew the first official contours of a Sui territory by dissociating them from the other 'barbarian' (Miao) populations of the region. The role of the classifications produced by Chinese ethnology in the Republican period in the future recognition of the Sui as a nationality is then highlighted, as is the founding role of the Sui scholar Pan Yizhi, of Sui ethnicity, who was briefly entrusted with the vice-presidency of the Sui autonomous district in 1957. The recent re-publication of his work, which was ill-treated during the Cultural Revolution, allows us to retrace the stages in the process of its creation. The paper concludes with a brief discussion of the instrumentalisation of this founding period for contemporary local development purposes.

Accelerating the exploration and development of deep ( > 1 000 m)coalbed methane (CBM) resources is an important way for the large-scale development of CBM and an important development direction in recent years. Guizhou Province is rich in CBM resources, with a large proportion of deep CBM resources. However, up to now, the geological research and exploration of deep CBM resources have not been carried out. Based on the geological background of CBM in Guizhou, this paper analyzes the geological characteristics and resource potential of deep CBM in Guizhou Province using a large number of CBM well test data. The research results show that the deep CBM resources in Guizhou are mainly distributed in many syncline units of the Liupanshui, North Guizhou and Zhina coalfields. Sedimentary differentiation and structural zoning lead to regional differences in the geological conditions of deep CBM reservoirs. The Liupanshui coalfield is characterized by “obvious overpressure, low temperature and high stress”, the Zhina coalfield is characterized by “overpressure, high temperature and low stress”, and the northern Guizhou coalfield is characterized by “overpressure, high temperature and high stress”. The permeability of deep CBM reservoir is low, and the permeability of 1 000 m deep will be generally lower than 0.1×10−15 m2. The CBM content of the coal reservoir is relatively high. The average CBM content of the middle-rank coal reservoir represented by the Liupanshui coalfield is 10.03 m3/t, and the average CBM content of the high-rank coal reservoir represented by the Zhina and Qianbei coalfields is 14.51 m3/t, and the deep supersaturation phenomenon is more obvious at 400 m. Based on the prediction model of free gas and adsorbed gas, considering the change of coal rack, it is predicted that the overall gas content in the deep part will further increase, and the supersaturation phenomenon will be more obvious, and the proportion of free gas will increase. At about 2000 m, the proportion of free gas will generally reach 10%−25%, and the proportion of free gas in medium-rank coal is higher than that in high-rank coal. On this basis, the geological resources of CBM in the key synclines of Guizhou Province with a depth of more than 2000 m are calculated. Based on the calculation results, the geological resources of CBM in Guizhou Province is 3.85 trillion m3, of which the geological resources of CBM in the depth of 1000 m reach 1.90 trillion m3, and the deep CBM resources in the Liupanshui and northern Guizhou coalfields account for a large proportion. Considering the scale and abundance of resources comprehensively, the development sequence is proposed. The Panguan-Tucheng-Zhaozihe-Jiupu'an syncline and the Gemudi syncline are the preferred development units. The above synclines are large gas fields with high abundance.

China is rich in karst resources and famous for its karst landscape. As a part of karst, the popularity of red karst is obviously low and has received little attention; moreover, the related scientific research and tourism development are relatively immature. Therefore, this paper takes the red karst in Tongren, Guizhou as the research object, analyzes the characteristics and causes of the red karst, comprehensively evaluates its landscape value, and puts forward development strategies and protection suggestions. Through the above research, the following three research results are obtained. (1) On the basis of a field investigation and a literature review, the geographical situation, background, and landscape characteristics of the red karst landform and its surrounding areas in Tongren City were investigated in detail. It forms isolated peaks, rock walls, protruding rocks, stone pillars, and other forms. The most prominent features of the red karst landscape in Tongren City are that the color is red and white, and the shape is concave and convex in order. (2) Geochemical test and structural data collection and analyses of the collected samples were performed. The obtain concave layer rock is dolomitic limestone, and that convex lay rock is argillaceous dolomitic limestone. Because the convex layer rock sample is high in silicon element content, the convex layer rock sample is not easy to be weathered, is rich in clay mineral, and is not easy to be corrode; the convex layer rock sample gradually protrudes with the passage of time to form an uneven shape. The red karst landform is developed in either the rock stratum or tectonic zone with moderate tectonic deformation intensity. First, the formation of a single-layer honeycomb morphology requires that the rock stratum is subjected to a sufficient horizontal compressive stress at a certain burial depth. Second, it is necessary to widely exist in areas with relatively gentle rock formation occurrence; too strong of a structural deformation will make the rock formation occurrence steep, which is not conducive to the occurrence of differential dissolution between adjacent strata. (3) Through the construction of an evaluation index system, the red karst in Tongren City is evaluated, and it is concluded that the geological heritage value is high, and the development and utilization conditions are weak. The conclusion of this article is a supplement to the geological and geomorphological system characteristics of southern karst. From the perspective of world natural heritage, the study enriches the academic evidence of red karst and enables its exemplary role to be well played. From the perspective of the tourism development value, more people should be made aware of the diverse types of karst landforms, which provide experience and suggestions for the value of landforms, tourism resources, and tourism development in similar areas.

In recent years, several moderate earthquakes with great influence have occurred in Guizhou Province. Guizhou people pay more attention to earthquakes and have an unprecedented demand for earthquake knowledge. In order to improve the public’s ability to deal with earthquake disasters, combined with the current practices of popular science propaganda, the paper puts forward some thoughts and suggestions on the development of popular science propaganda for earthquake prevention and disaster reduction in Guizhou Province.

There are many species of terrestrial Mollusca with rapid reproduction rates, a wide distribution range, and a large population. They are not only an important wildlife resource but also an important component of biodiversity. Previously, basic research has been conducted on the species diversity and distribution of terrestrial Mollusca in some nature reserves in Guizhou and Yunnan. The existing sample data of terrestrial Mollusca in Guizhou and survey results from Guiyang, Libo, and Xishui from July 2019 to December 2020 listed 316 species and subspecies (including 13 undefined species) belonging to two subclasses, four orders, 20 families, and 76 genera in Guizhou Province. From the perspective of species composition, the dominant family is Cyclophoridae, with 16 genera and 71 species; the second most dominant family is Bradybaenidae, with 15 genera and 61 species, followed by Helicinidae and Cochlicopidae with one genera and one species. The dominant species are Kaliella cavicola, Bradybaena similaris, Diplommatina herziana, Diplommatina consularis, Chamalycaeus nanus, and Plectotropis pseudopatula. From the perspective of geographical distribution, terrestrial Mollusca are the most abundant in the central region of Guizhou, with 17 families, 54 genera, and 170 species. The areas with the second greatest abundance of terrestrial Mollusca are the sub-subtropical humid areas in southern Guizhou and the sub-subtropical areas in southwestern Guizhou, with 18 families, 56 genera, and 152 species and 17 families, 57 genera, and 150 species, respectively. There are only 10 families, 18 genera, and 27 species in the eastern area of Guizhou. Similarity analysis of species in different regions of Guizhou Province showed that the species composition of terrestrial Mollusca in the southern area, northern area, and southwestern area of Guizhou is similar, whereas the species composition of terrestrial Mollusca in the eastern area of Guizhou is markedly different from that of other regions. This paper discusses the species and distribution pattern of terrestrial Mollusca in Guizhou Province and their resource characteristics to provide a scientific basis for the protection and rational utilization of terrestrial Mollusca resources and to further enrich the research data of terrestrial Mollusca in China.

In recent years, due to adverse geological conditions, intense human engineering activities, and extreme weather conditions, catastrophic landslides have frequently occurred in southwest China, causing severe loss of life and property. Identifying the kinematic features of potential landslides can effectively support landslide hazard prevention. This study proposes a remote sensing identification method for rotational, planar traction, and planar thrust slides based on geomorphic features as well as vertical and slope-oriented deformation rates. Rotational landslides are characterized by similar vertical and horizontal deformation rates, with vertical deformation mainly occurring at the head and gradually decreasing along the slope, while horizontal deformation mainly occurs at the foot and gradually increases along the slope. As for the planar slide, the dominant deformation is in the horizontal direction. It is further classified into the planar traction and planar thrust types according to the driving position. The vertical deformation of planar traction slides is concentrated at the foot, while the vertical deformation of planar thrust slides is concentrated at the head of the landslide. We identified 1 rotational landslide, 10 planar traction landslides and 10 planar thrust landslides in the basalt weathering crust area of Guizhou. Field investigations of three landslides verified the method’s accuracy. Combining two-dimensional rainfall and time-series deformations, we found that there is a significant positive correlation between landslide deformation acceleration and precipitation. The landslide kinematic identification method proposed in this paper overcomes the shortcomings of the inability to accurately characterize landslide motion by line-of-sight displacement and realizes the non-contact identification of active landslide motion patterns, which is an essential reference value for geological disaster prevention and control in the study area.