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1.
This paper further develops the ideas of V. B. Sochava’s Siberian school of thematic mapping concerning an integral approach in generating synthesis and assessment maps of the habitat on objective grounds confirmed by quantitative calculations. Maps of the natural environment display the invariant structure of the sites of a territory and their variable states. Integral indicators of the state of environment combine differentquality spatial information on the geographical location of the sites having regard to the scientific principles of qualimetry. An unbiased calculation of integral indicators is ensured through the use of the method of principal component analysis. The first principal component characterizes a maximum of variation in information on the geosystem, and the second component refers to a stable environment background. Their difference for each location corresponds to the potential of geosystem variability. The resulting integral indicators are displayed on assessment cartograms. The entire array of independent principal components is used for a classification of geosystems using the method of k-means clustering to create the typological map of the territory. Calculations are based on data for forest management of the Slyudyanka Leskhoz within the boundaries of the Slyudyanka municipal district of Irkutsk oblast. The territorial norm of the geographical environment corresponds to geosystems of the mountain-taiga belt of the Siberian stone pine and larch taiga on different-aspect slopes. Negative deviations from the norm are induced by high-mountain goletz and subgoletz geosystems on steep slopes, and positive deviations correspond to flat interfluves and gentle slopes.  相似文献   

2.
Presented are the technique and results of studying the landscape structure of the north-west of Western Siberia on the basis of the Hansen mosaic dataset consisting of elements covering the entire territory of the Earth. To study this area used a synthesis of classical methods of thematic system mapping as described in the doctrine of geosystems of V. B. Sochava, and automated interpretation of remote sensing data and mapping using GIS technologies. The method of geoinformational mapping of the landscape structure with the use of MultiSpec and Quantum GIS software programs for the purpose of drawing up real-time raster landscape maps is shown. In drawing up the map and the legend, the principle of geomic system-hierarchical representation of the territory as a complex multi-level “bottom-up” structure from topological-level geosystems (groups and classes of landscape facies) to regional-level geosystems (geoms, groups and classes of geoms) was used. Compilation of operational raster landscape maps of the north-west of Western Siberia involved multilevel automated interpretation of the Hansen mosaic dataset and mapping of areas (clusters) on images with different brightness characteristics, with the landscape structure of key areas and stationary physical and geographical profiles. A characteristic of this approach also implies using a dynamic classification of geosystems based on the study of their variable states. Such an approach permits a monitoring of changes in landscape structure and its areas and the intensity of anthropogenic impacts on forest and marsh landscapes, and determination of permissible pressure on geosystems in areas with high technogenic pressure of the oil and gas complex represented by the north-west of Siberia. An automated processing of data based on a supervised classification of territorial objects allows for the elimination of inaccuracies arising in visual image interpretation. Raster landscape maps can be used both for a further generation of vector maps and as a real-time information base for purposes of environmental management and protection.  相似文献   

3.
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4.
We consider some methodological principles of forecasting changes in the geom structure of the Prebaikalia’s territory under climatic warming. A forecast is made by using a GIS that was created on the basis of the landscape map for the southern part of East Siberia. The identified spatial connections of geoms, the characteristic altitudes at which each geom is located, and the location structures of geom units in altitude serve as a basis for forecasting.  相似文献   

5.
Results from investigating the geosystems of Cisbaikalia in its western and eastern parts (Primorskii Range and Barguzin Range, respectively) are presented. For studying three macroslopes of these mountain ranges (having an easterly aspect for the Primorskii Range and a westerly and south-easterly aspect for the Barguzin Range), the regional background and the main factors of the landscape differentiation of the study areas were analyzed. Structural features of topological geosystems are revealed, and large-scale maps of key areas are compiled (at a scale of 1:50 000). Maps of the landscape-typological structure were created on the basis of the structural-dynamic and facies analysis of landscapes. It is established that the main factors influencing the landscape diversity are the aspect and steepness of the slopes, the composition and structure of rocks, the absolute height, the amount of atmospheric precipitation, and anthropogenic impacts. It is determined that the influence of the lithomorphic factor is widespread throughout the study areas, the hydromorphic factor is also important, the cryomorphic factor occurs additionally in the goletz zone, and the xeromorphic factor is only observed on the Baikal Range and on the coastal plain in some areas of Priolkhonie. The dynamic aspect of the landscape structure and the relationships between geosystems are displayed in map legends.  相似文献   

6.
Calculations of the activity indices and species richness of belt-zonal elements of the flora of dark-coniferous forests have been done in order to reveal the presence of climatogenic changes. It was found that there is an increase in activity of the species of the dark-coniferous belt-zonal group peculiar to these forests. It is suggested that this phenomenon is associated with current climate warming. It is concluded that with increasing climate warming and with the persisting tendency for its humidification, in the lower belt of the mountains there will be taking place an enhancement in the landscape role of dark-coniferous forests through succession from light-coniferous forests to them.  相似文献   

7.
A unified methodological approach was used to study the soil zoocenoses of uneven-age industrial areas of the Kovykta gas and condensate field. Regeneration of the soil-biotic block is characterized by sequential changes in quantitative characteristics, and in the taxonomic and functional structure of invertebrate communities. The study revealed distinguishing characteristics of the progressive successions of drastically disturbed mountain-taiga geosystems, and the factors that are responsible for the direction and duration of the individual successions.  相似文献   

8.
An analysis is made of the data from experimental investigations into the influence of fires on changes in the soil-protective functions of Siberian stone pine and pine forests in the southern part of the central ecological zone of the Baikal natural territory. The study revealed a negative influence of ground fires of the litter-humus type on changes in reserves and qualitative functional composition of forest litter and its moisture retention capacity as well as in water-physical properties of soils. Quantitative indices are provided for the liquid and solid overland runoff forming in burnt-over areas, depending on slope steepness, and on the intensity and temporal remoteness of past fires.  相似文献   

9.
云南陡坡地优化利用若干问题研究—以滇西北地区为例   总被引：1，自引：0，他引：1  
云南陡坡垦殖较为严重,滇西北地区尤为突出。主要原因有宜耕地缺乏、社会经济发展滞后、粮食单产低、人口增长较快、交通不便等。陡坡垦殖导致植被破坏、土壤侵蚀;环境变劣,部分地区失去生存条件;灾害频繁,威胁中下游地区生命和财产安全。退耕还林是一项系统工程。工作尚未大规模开展之前,应认真落实应退耕地面积和退耕还林地块,积极解决群众温饱,减轻土地压力。退耕还林规划应与区域发展规划协调一致;建立农林复合系统,实现陡坡地优化利用;组织技术培训,建立技术保障系统;发展交通事业,改善生产生活条件。  相似文献   

10.
Using an ingenious cartographic method, for the Baikal natural territory we have developed a benchmark network that includes 18 tracts (0.47% of the territory under consideration). Special-purpose ground-based surveys of the selected tracts showed that such a network fully reflects the landscape diversity on the level of geoms, the phytocenotic diversity, and the species diversity of the regional biota.  相似文献   

11.
An analysis made of the worldwide existing geoinformation systems (HydroSHEDS, CCM, Ecrins, WBD, etc.) suggests that there are as yet no models of adequate quality for the basin boundaries of small rivers in the European part of Russia. For the territory of the European part of Russia with a total area of more than 4 mln. km2 the GIS technology tools were used to construct the electron vector map of river basins and their interbasin spaces. The map thus obtained displays the basins of first-order rivers for a given level of generalization (sc 1:1 000 000). The GMTED2010 model was used as the digital elevation model. A total of 63 553 basin geosystems were identified on the map, averaging 68 km2 in area. Accuracy verification of identifying the basin boundaries showed a good agreement of areal and geometric characteristics of the method used with expert approach. In test areas, the men difference of the indicators of the area of the basins identified automatically and by use of the expert approach made up 3.6%. For areas with weakly dissected lowland topography this error does not exceed 5% while it is about 2% in areas with relatively dissected elevated topography. The basin geosystems thus identified are operational-territorial units with respect to which the geospatial data base is generated to characterize the natural-resource potential of the European territory of Russia. An example is provided for the generation of the geospatial database containing hydrological information covering 1763 hydrological stations collecting streamflow data.  相似文献   

12.
The key aspects of reindeer ecology within the Konda river basin are considered. The study revealed the factors governing the characteristics of calving reindeer pastures determined by the structure of forest-bog landscapes of a different generalization level. A deficit of such pastures is regarded as the factor of differentiation of reindeer groups with respect to migrants and residents. It is shown that the individual geocomplexes have a multifunctional role. Of particular significance among them are the aufeis glades with outcrops of salt-saturated groundwater, and the dark-coniferous forests along river valleys rich in epiphytic lichens (beard lichens).  相似文献   

13.
The long-term vegetable matter dynamics in geosystems of the Nazarovskaya forest-steppe is considered. The differences in phytomass reserves for the facies of the Berezovskii area are demonstrated. The study revealed a clear-cut rhythmic behavior of variability in phytomass and its life forms which is attributed to the bioclimatic situation not only in a current year but also in preceding years. It is shown that anthropogenically disturbed lands are experiencing a progressive succession which manifests itself in successive changes of the grass stand.  相似文献   

14.
Presented is the predictive topo-ecological concept, based on empirical-statistical models of geosystems. Using the geosystems of the Volga basins as an example, this study considers the mechanisms of local and regional response to the global warming expected in the 21st century. A general process of “savannization” of mixed and broad-lived forests is predicted for the Middle band of the Russian Plain with the development of the thermoarid climatic trend. The prognostic non-representativity of the known palaeographical scenarios of the warm epochs during the Pleistocene and Holocene is demonstrated.  相似文献   

15.
The formative stages of the geosystem mapping methodology are outlined. It is determined that the early stages of geosystem mapping showed a continuity of the ideas of geobotanical mapping: concerning the hierarchical structure of the phytosphere, and the invariant and the variable states of plant communities. It was found that geosystem mapping involves integrating the facies according to structural and structural-dynamic indicators differing from a traditional typization. Data were generalized having regard to the assignment of the facies to a particular landscape area. Use was made of the facies categories of optimal, limited and reduced development caused by a difference in their structure and biotic productivity. It was determined that a next mapping stage implied identifying the dynamic categories and geosystem state variables associated with one primary geomer regarded as the parent core. The map legend was based on the characteristics of the relief and vegetation. The absence of other indicators has limited the possibilities of using the map to solve forecasting problems. It was established that at present, given a significant body of landscape data, there is almost no research devoted to the cartographic solution of the problem of assessing changes in the natural environment. There is a need for mapping of the structural, dynamic and genetic uniqueness of geosystems and to explain their diagnostic features in all crucial components. We determined that the current stage of mapping should be focused on solving the problem of geographic map-based forecasting. For solving the forecast issues, we identified the features of structural-dynamic and evolutionary transformations of geosystems, their stability, and the direction of transformation under the influence of various factors. The methodology and stages of geosystem mapping are suggested.  相似文献   

16.
Water is well established as a major driver of the geomorphic change that eventually reduces mountains to lower relief landscapes. Nonetheless, within the altitudinal limits of continuous vegetation in humid climates, water is also an essential factor in slope stability. In this paper, we present results from field experiments to determine infiltration rates at forested sites in the Andes Mountains (Ecuador), the southern Appalachian Mountains (USA), and the Luquillo Mountains (Puerto Rico). Using a portable rainfall simulator–infiltrometer (all three areas), and a single ring infiltrometer (Andes), we determined infiltration rates, even on steep slopes. Based on these results, we examine the spatial variability of infiltration, the relationship of rainfall runoff and infiltration to landscape position, the influence of vegetation on infiltration rates on slopes, and the implications of this research for better understanding erosional processes and landscape change.Infiltration rates ranged from 6 to 206 mm/h on lower slopes of the Andes, 16 to 117 mm/h in the southern Appalachians, and 0 to 106 mm/h in the Luquillo Mountains. These rates exceed those of most natural rain events, confirming that surface runoff is rare in montane forests with deep soil/regolith mantles. On well-drained forested slopes and ridges, apparent steady-state infiltration may be controlled by the near-surface downslope movement of infiltrated water rather than by characteristics of the full vertical soil profile. With only two exceptions, the local variability of infiltration rates at the scale of 10° m overpowered other expected spatial relationships between infiltration, vegetation type, slope position, and soil factors. One exception was the significant difference between infiltration rates on alluvial versus upland soils in the Andean study area. The other exception was the significant difference between infiltration rates in topographic coves compared to other slope positions in the tabonuco forest of one watershed in the Luquillo Mountains. Our research provides additional evidence of the ability of forests and forest soils to preserve geomorphic features from denudation by surface erosion, documents the importance of subsurface flow in mountain forests, and supports the need for caution in extrapolating infiltration rates.  相似文献   

17.
Using the biogeocenoses of taiga geosystems as an example, we employed the method of correlation analysis and the technique for analyzing the main components to demonstrate that a relative altitude is a complex indicator of serialness of landscape-level geosystems, reflecting not only the particular geographical signatures but also a certain system of conjugation of the portions of landscape and the force of spatial and typological connections that causes the concrete facies to deviate from zonal normal. Complex indicators: the main components, and the correlation and regression coefficients, were used to reveal a functional correlation of the sets of BGC attributes between themselves and with a relative altitude of the location.  相似文献   

18.
《Geomorphology》2006,73(1-2):149-165
Manjiya County on the Ugandan slopes of Mount Elgon is a densely populated mountainous area where landslides have been reported since the beginning of the twentieth century. The numerous fatalities and the damage done during the extreme rainfall events of 1997 to 1999 drew attention to this phenomenon. In order to better understand the causal factors of these landslides, 98 recent landslides in the study area, mostly debris slumps, were mapped and investigated. Together, they displaced 11 millions m3 of slope material. Statistical analysis shows that landslides dominate on steep concave slope segments that are oriented to the dominant rainfall direction (northeast) and at a relatively large distance from the water divide. Based on landslide occurrence and impact, four different zones can be distinguished within the study area. Causal factors as well as landslide characteristics differ greatly between the four zones.Besides the fact that steep slopes, high rainfall and typical soil properties and stratification turn Manjiya into an inherently unstable area, human interference cannot be neglected. Whereas deforestation has reduced the stability of the shallow soils on the eastern slopes of the study area, the excavation of slopes, mainly for house building, is an important destabilizing factor for the western slopes. The growing population density not only increases the risk on damage, but hampers the search for solutions for the landslide problem as well.  相似文献   

19.
Cryogenic block streams consist of a stream of rocks superficially resembling a stream deposit but lacking a matrix, usually occurring on a valley or gully floor or on slopes that are less steep than the maximum angle of repose of coarse sediments. They are usually formed on perennially frozen ground, but can also occur as relict landforms. There are three main active kinds forming today, viz., Siberian and Tibetan dynamic rock streams and lag block streams. During their formation, the blocks in the active Siberian and Tibetan dynamic block streams move downslope at up to 1 m/a. They are forming today on the Tibetan Plateau and in the more arid parts of south-central Siberia, although the processes involved in the movement are different. In the case of the Tibetan type, individual blocks slide downslope over the substrate in winter on an icy coating in areas of minimal winter precipitation. The Siberian type develops in areas of 15–80 cm of winter snow cover and an MAAT(mean annual air temperature) of-4 °C to-17 °C. The movement is due to creep of snow and ice and collapse of the blocks downslope during thawing. Lag block streams are formed by meltwater flowing over the surface of sediment consisting primarily of larger blocks with a limited amount of interstitial sediment. The erosion of the matrix is primarily in the spring in areas of higher winter precipitation on 10°–30° slopes. The blocks remain stationary, but the interstitial sediment is washed out by strong seasonal flows of meltwater or rain to form an alluvial fan. The boulders undergo weathering and become more rounded in the process. Lag block streams can also develop without the presence of permafrost in areas with cold climates or glaciers. Block streams also occur as relict deposits in older deposits under various climatic regimes that are unsuitable for their formation today. An example of relict lag block streams with subangular to subrounded blocks occurs in gullies on the forested mountainsides at Felsen in Germany, and is the original "felsenmeer". Similar examples occur near Vitosha Mountain in Bulgaria. The "stone runs" in the Falkland Islands are examples of the more angular relict lag block streams. In both Tasmania and the Falkland Islands, they mask a more complex history, the underlying soils indicating periods of tropical and temperate soil formation resulting from weathering during and since the Tertiary Period. Block streams have also been reported from beneath cold-based glaciers in Sweden, and below till in Canada, and when exhumed, can continue to develop.  相似文献   

20.
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