Том 37, № 3 (2016)

The role of East, South and Central Asia in the world development is shown. The current per capita availability of water resources is calculated for the countries of the region. It is found that on the whole for the territory under investigation the availability of water resources is more than twice as small as the world’s average indicator and that more than 1.5 billion people live in conditions of water stress and deficit. It is pointed out that by the year 2010 more than 70% of the population lived in conditions of high pressure on water resources, and 225 million people lived under very high and critical water stress conditions. The current pattern of water use in the countries of Asia is calculated, the dominant role of the agrarian sector is identified. An analysis is made of the measures for increasing the water availability level of the population and the economy: an increase in agricultural productivity of water resources, waste water reuse, use of saline waters, and the construction of reservoirs. Attention is given to an active construction of dams by China in the upper reaches of the Mekong which is causing distrust and tension in downstream countries. Statistical data on cooperation and conflicts in international basins of Asia is reported. It is shown that in the 20 th century the basins of the Indus and Ganges rivers experienced the largest number of water conflicts as compared to all the international basins of the world; information regarding an acute struggle for water resources in Central Asia is also provided. It is concluded that in view of an ever increasing deficit of water resources, cooperation is the only alternative for Asian countries.

Presented is a detailed characterization of the present state and pollution of soil cover in the influence area of the Dzhidinskii tungsten-molybdenum plant which takes into consideration the spatial geological inhomogeneity and the functional purpose of urban territories. As part of the investigation, we determined the content levels of heavy metals and metalloids in background soils, and the elements which are the main pollutants of urban soils in the zones of different functional purposes, ascertained the degree of technogenic geochemical transformation of soil cover in the city of Zakamensk, and identified the leading soiland landscape-geochemical factors for accumulation of heavy metals and metalloids in the urban topsoil (0−10 cm) horizons. An assessment was also made of the ecological hazard of soil pollution by a set of heavy metals and metalloids in the main functional zones of the city. A soil-geochemical survey was carried out, and the ICP-MS method was used to determine the total content levels of 14 heavy metals and metalloids of hazard classes I−III as well as Be, Sn, Cs and Bi. The elements were determined, which are the main pollutants of the soils in Zakamensk: W, Bi, Cd, Pb and Mo. The study revealed a need to take into account the metallogenic specific character and geological inhomogeneity of the area by using the local coefficients of concentration (EF_l) and dispersal (DF_l) which must be calculated not with respect to the average regional background but from the individual (for each parent material) background value in order to more accurately determine the degree of technogenic geochemical transformation of soils, and the ecological hazard of pollution. It is suggested that the ecological hazard should be assessed on the basis of the Integrated Pollution Index (IPI) which is calculated with respect to the world’s average concentrations of heavy metals and metalloids in soils and takes into account hazard classes of elements.

We investigated the influence of deep forced temperature convection on aeration of the bottom water layer in the pelagic zone of Baikal. Temperature T (± 0.002°C) and oxygen O₂ concentration (± 0.01 mg/L) were measured by using the SBE-25 probe with the SBE-43 oxygen sensor in May-July 2006−2007 and 2009−2013. Oxygen input into the bottom layer with cold intrusions was determined for 79 cases. The study revealed a quantitative correlation between the heat deficit and the rise in oxygen content in the bottom layer during cold intrusions. This correlation was used to reconstruct the values of intrusion aeration of the bottom layer during 1993−2005. It is ascertained that the intrusion-caused 2006−2013-average oxygen input into Baikal’s bottom layer is virtually close to the annual oxygen demand for oxidation processes in the water column and bottom sediments. In the southern and middle parts of Baikal, intrusion-caused input of oxygen corresponds to a higher rate of its demand (4.5−4.6x10^-4 mg/L per day). A slight increase in oxygen concentration was detected in the bottom layer of the South and Middle Baikal and a slight decrease in the bottom layer of North Baikal during 1993−2013.

Presented are the results from pedolithological investigations and reconstructions of the naturalclimatic events in the Early Holocene (radiocarbon age 10.3−8 ka; calendar age 11.7−8.8 ka) on the coast of Middle Baikal, based on data obtained by studying the structure, composition and properties of subaerial deposits and soils in terrestrial sections. A study was made of the numerous soil profiles and sections of geoarchaeological sites. The investigation revealed common features in the layered structure of the Early-Holocene portion of the terrestrial sections and evidence of climate warming represented by buried soils, signals of a cooling in the form of cryogenic fissures, and signals of drying in the form of aeolian drifts and evidence of deflation. It is shown that the Early Holocene was the time of cardinal changes in the nature of subaerial sedimentation (calcareous deposits were replaced by noncalcareous deposits) and the pedogenesis. Considerable cold storage from inherited permafrost and humidification of soils and earth materials with moisture from the thawing of permafrost were responsible for the specific character of soil formation, and for the spread of forest vegetation under a rather low atmospheric humidity. The phases of climate warming were accompanied by an intensification of soil formation with the production of soils of two types: early boreal, and boreal. Deluvial, colluvial and sometimes (in Priol’khonie) aeolian deposits accumulated during the cooling phases (Late Preboreal and Late Boreal). Small cryogenic fissures were generated. The issues of man’s adaptation to the cardinally changed natural conditions at the turn of the Pleistocene and Holocene and over the course of the Early Holocene are associated with the problem of Baikal’s water level and human settlement on its shores. The Lake Baikal stage at the end of the Late Neopleistocene was lower than at present; during the Early Holocene it was rising to reach at the late-boreal period the present-day level (or even exceeded it). The rises of Baikal’s stage at the Mid- and Late-Holocene period were causing scouring and destruction of the Early-Holocene sites that were located at lower elevations.

We discuss the issues related to the human colonization of the Tuva landscapes in the Scythian time. An analysis is made of the spatial and landscape confinedness of archaeological sites having regard to the Late-Holocene rhythms of climate change in the mountains. For the historical-landscape analysis the MapInfo 12.0 GIS technologies were used in compiling the landscape map of the Tyva Republic, the scheme of physical-geographical regionalization and the schematic map of spatial distribution of archaeological sites from the Scythian time. The then most developed landscapes include the steppe mountain-valley and forest-steppe low- and mid-mountain landscapes, which was associated with the main economic sector, namely nomadic stockbreeding. The culture of the Scythian time existed under a colder and more humid climate than at present. An increase in humidity in originally dry areas led to an increase in steppe vegetation productivity growing in depressions and on slopes of mountain ranges. These factors created favorable conditions for the development of nomadic stockbreeding. A spatial analysis of the distribution of archaeological sites in the physical-geographical provinces of Tuva intimates that depression landscapes were colonized mostly in the Scythian time. The Tuvinian depression province (the archaeologically richest area of Tuva) and the Ubsunur depression account for 52 and 21% of the sites, respectively. The mountain landscapes were colonized to a considerably lesser extent; the largest number of sites are located in the Western-Tuva mountain province. In the Scythian time, the cores of development of the Tuva territory were represented by the intermontane depressions (Tuvinian and Ubsunur), the connections between which were provided by a small number of large valleys and mountain passes.

The dynamics of land use in Russkii Island is considered for the period from 2007 to 2014, and some issues of its future development are analyzed. The areas of lands of different categories and the maps of land use on the Sapernyi Peninsula are provided for different time spans. It is established that the implementation of the program of the preparation of Vladivostok for APEC Summit 2012 led to a substantial change in the land use pattern in Russkii Island: the area not involved in the economic turnover decreased by 5.09%, the zone of production, engineering and transport infrastructure increased by a factor of 21.5, and the share of lands for recreational purposes increased more than twice. It is shown that recreational activities implying a decrease in the share of lands not drawn into the economic turnover by more than a factor of 5 must become the dominant kind of land use (according to the program of development of Vladivostok). Attention is focused on the issue related to the creation of the territory of priority socioeconomic development in Russkii Island through the use of private-state partnership mechanisms. It is pointed out that the implementation of the development plans for the island is delayed, in spite of the legislative and financial support from federal and regional authorities. Emphasis is placed on the need to develop the program of comprehensive substantiation, modeling and forecasting of the development of Russkii Island in the interests of the sustainable functioning of the natural-economic system.

We examine the phenomenon of “collapsed” states by using, as an example, Somalia that is being faced with a vast array of problems: collapse of state institutes, civil war, separatism, terrorism, radical Islamism, and piracy. It is found that clannishness and tribalism of Somali society are complicating the process of political settlement and national reconciliation. It is pointed out that some of the tribes and groups, including under the action of external forces, are actually forming the country’s political space. It is shown that the pseudo-state entities in Somalia are unstable, and their boundaries of “flowing” so that they are incapable of exercising a full control over the territory. It is emphasized that the problem of Islamic extremism can be treated as deriving from failure of the state institutes; the peak of activity and territorial expansion of Islamist groups in the country is now in the past, and the area of their activity is bounded by the area inhabited by the Somali ethnos. It is found that the piracy problem is determined by the geographical location of Somalia, and its solution is impossible without the reestablishment of the state institutes and the economic system of the country. Two potential cores of reestablishment of Somali statehood have been revealed: Federal Government in Mogadishu as well as the Autonomous Republic of Puntland. It is forecasted that the international community will be gradually recognizing the Republic of Somaliland. It is concluded that the federalization of the country as declared by authorities is formal in character but yields first results implying that the negotiation process between the groups of clans has been led into a political channel.

We investigate the additionality of the principles of geoecological ethics and ethical geography from the perspective of the manifestation of the norms of human activity in the natural environment. Geoecological ethics is based on the through principles of sustainable development and responsibility for breaches of different-quality norms existing in nature, economy and society, and on social relations considered in different systems with due regard for the characteristics of geographical environment. The degree of responsibility is measured in dimensionless indicators of reliability (dependability) theory, the integrated hazard of activity with natural restrictions on the action on geosystems and departures from normative states. Ethical geography generates landscape-cultural norms of implementation of different kinds of activity on a territory. The general ethical laws and quantitative models and methods for responsibility assessment are special interpretations of the notions and axioms of general system theory adopted as the norm of organization of knowledge. The principles of geoecological ethics manifest themselves as a result of the interpretation of the general laws of ethics via the geohistorical environment, primarily in the form of responsibility for a departure from the environment-caused norms of activity. Ethical geography implies responsibility for the reliability of knowledge of the generally significant norms of the state and allowable changes in environment. A violation of geoethical norms and nature management normative will necessarily lead to negative changes in the living conditions of man and society.