SPACE IMAGERY IN THE STUDY OF SOIL COVER IN THE KUDA RIVER BASIN

2000 ◽  
Vol 37 (3) ◽  
pp. 189-197
Author(s):  
T. V. Keyko
Keyword(s):  
Author(s):  
Antonio Conceição Paranhos Filho ◽  
Alberto Pio Fiori ◽  
Leonardo Disperati ◽  
Cristiane Lucchesi ◽  
Alessandro Ciali ◽  
...  

O ambiente SIG (Sistema de Informações Geográficas) é o ideal para integrar dados, informações e cartas de naturezas diferentes. Por exemplo, dados climáticos e cartas topográficas ou de solos podem ser analisados em conjunto, levando toda a informação para uma base comum, o que permite a sua integração e uso. A Equação Universal de Perdas dos Solos (EUPS ou USLE) é atualmente utilizada, com sucesso, como uma forma para a avaliação da perda dos solos por erosão laminar e foi aplicada para a Bacia do Rio Taquarizinho (ao Sul de Coxim, Mato Grosso do Sul), região que apresentou grandes modificações no tipo de uso e ocupação do solo no período analisado. Neste trabalho são apresentados os parâmetros envolvidos com a USLE, alguns obtidos da digitalização de cartas temáticas e tabelas como de Erosividade das chuvas (R), Erodibilidade do solo (K) ou Uso e Manejo do Solo e Práticas Conservacionistas (CP) e outros, como Comprimento (L) e Declividade de vertentes (S,) obtidos em ambiente SIG, através de dados topográficos. O ambiente SIG permitiu a completa integração entre os dados para a obtenção dos parâmetros da USLE e os resultados. Para a Bacia do Rio Taquarizinho a USLE foi aplicada em três diferentes momentos: 1966, 1985 e 1996. Esta aplicação multitemporal mostrou a tendência evolutiva do processo erosivo na região. Para os valores absolutos da taxa de erosão laminar dos solos, de 1966 a 1996, em alguns locais, o desmatamento implicou num aumento da taxa de erosão laminar dos solos em mais de 50 vezes. As perdas médias anuais de solo por erosão laminar foram representadas por valores médios, para toda a Bacia do Taquarizinho, de 4,44 ton/ha. para 1966, de 5,53 ton/ha. para 1985 e de 8,65 ton/ha. para 1996. MULTITEMPORAL EVALUATION OF SOIL LOSS IN THE TAQUARIZINHO BASIN, MATO GROSSO DO SUL - BRAZIL Abstract The GIS - Geographic Information System environment is ideal for integrating data, information and different kinds of maps. For example, climate data and topographic or soil cover maps can be analyzed together, bringing all the information into a common base, thus permitting integration and use. The Universal Soil Loss Equation (USLE) is currently used successfully as a form of evaluating soil loss via laminar erosion, and it was applied to the Taquarizinho River Basin (to the south of Coxim, Mato Grosso do Sul State), a region which showed great changes in the type of use and occupation of the soil during the period analyzed. In the present work are presented the parameters involved in the USLE, some obtained from the digitalization of thematic maps and tables, such as the Rain Erosive Potential (R), Soil Erodability (K), and Cover and Management of the Soil and Conservation Practices (CP), and others, such as Length (L) and Slope Declivity (S), obtained from the GIS environment, from topographic data. The GIS environment permitted a complete integration between the data used to obtain the USLE parameters, and the results. For the Taquarizinho River Basin, the USLE was applied to three different periods: 1966, 1985 and 1996. This multi-temporal application showed a tendency of evolving erosion in the region. Calculations of the absolute values of rates of laminar erosion of the soils indicate that deforestation has lead to an increase of more than fifty times in such erosion, from 1966 to 1996. The mean annual losses of soil from laminar erosion for the entire Taquarizinho River Basin are calculated to have been 4.44 ton/ha in 1996, 5.53 ton/ha in 1985, and 8.65 ton/ha in 1996.


2017 ◽  
Vol 921 (3) ◽  
pp. 36-42
Author(s):  
D.N. Lopatina

The soil cover of Osa river basin is described in the article, its variety caused by features of a geological structure, relief, climate, vegetation and anthropogenous impact is revealed. Set of factors of soil formation which gives prerequisites for forming of special types of the soils which aren’t fitting into traditional representations of zone types of a taiga and forest zone – chernozems, dark-humic and other soils under steppe vegetation is studied. In total three trunks, nine departments, 27 types and 46 subtypes of soils are allocated. It is established that the main area (more than 7 0 %) is provided by the soils entering into departments of the accumulative and humic, organo-accumulative and textural differentiated soils, agrozyom, and the insignificant territories are busy with full-height types of soils of structural and metamorphic department, litozyom, abrazyom, alluvial. 37,3 % of the general territory of a research occupy agricultural holdings, from them about 12,8 % are used now, 87,2 % are in abandon condition. The map «Soils of Osa River Basin» is provided in the article.


Author(s):  
П.Н. Уланов ◽  
А.Н. Романов ◽  
Д.Н. Трошкин ◽  
И.В. Хвостов

Author(s):  
Marianna Shipka

Ensuring the ecological sustainability of the territory is possible in the case of the optimal ratio of different types of lands. In particular, it is important to have sufficient areas of eco-stabilizing lands (forests, meadows, protected areas, etc.). Of great importance are the features of land use in coastal areas, areas with high steep slopes and areas with soils susceptible to degradation. Ecologically sustainable land use can reduce the risk of soil degradation processes, provide an optimal microclimate, good hydrological conditions and promote the protection of small rivers. To provide recommendations for improving the structure of land use in the Poltva river basin, a map of optimization of the structure of land use using the ArсGIS 10.0 program was drawn up. For this purpose, a map of slope steepness was constructed, an interpretation of space images was made to compile a map of land use structure and a map of the soil cover was digitized. As a result of the analysis of the map of land use structure the peculiarities of the ratio of types of lands in different parts of the studied territory by integral indicators are determined. The coefficients of anthropogenic load, ecological stability of land use, ecological stability of landscapes, ecological balance and others are calculated. Areas with different degrees of anthropogenic transformation of lands are identified. The relationship between the peculiarities of natural conditions (geological structure, relief, soil cover) and land use of the territory is analyzed. As a result of overlapping maps of slope steepness, soil cover and land use, areas with different risk of soil degradation processes and plowed coastal areas were identified. The map of land use structure optimization is compiled according to the method of allocation of ecological and technological groups of lands. According to this technique, lands are differentiated by the steepness of the slopes. The proposed optimization of land use involves the use of phytomeliorative and agrotechnical measures: plowing across the slope, soil-protective crop rotations, the creation of forest belts, land conservation, etc. Recommended optimization measures include the withdrawal from agricultural cultivation of peatlands, steep slopes, floodplains, hollows, coastal protection zones of rivers and streams. The implementation of the proposed optimization measures will reduce plowing, increase the share of eco-stabilizing lands and improve the integral indicators characterizing the ratio of different types of lands. A compiled map of land use structure optimization can be used for land management and environmental activities. Key words: anthropogenic load, land use, ecological and technological groups of lands, river basin, optimization, Bug river.


2015 ◽  
Vol 48 (3) ◽  
pp. 231-239 ◽  
Author(s):  
A. N. Bugaets ◽  
N. F. Pshenichnikova ◽  
A. A. Tereshkina ◽  
S. M. Krasnopeev ◽  
B. I. Gartsman

2019 ◽  
Vol 60 (3) ◽  
Author(s):  
Б.С. Керімбай ◽  
К.М. Джаналеева ◽  
Н.Н. Керімбай
Keyword(s):  

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