CA-Markov prediction modeling for the assessment of land use/land cover change in two sub-basins of the Tocantins-Araguaia River Basin

被引:2
|
作者
dos Santos, Wharley P. [1 ]
Acuna-Guzman, Salvador F. [2 ]
de Oliveira, Paulo T. S. [3 ]
Beniaich, Adnane [4 ]
Cardoso, Dione P. [1 ]
Silva, Marx L. N. [1 ]
Curi, Nilton [1 ]
Avanzi, Junior C. [1 ]
机构
[1] Fed Univ Lavras UFLA, Dept Soil Sci, BR-37200900 Lavras, MG, Brazil
[2] Univ Puerto Rico Mayaguez, Dept Agr & Biosyst Engn, Mayaguez, PR USA
[3] Univ Fed Mato Grosso Do Sul UFSM, Fac Engn Architecture & Urbanism & Geog, BR-79070900 Campo Grande, MS, Brazil
[4] Univ Mohammed VI Polytech UM6P, Coll Agr & Environm Sci CAES, Agr Innovat & Technol Transfer Ctr AITTC, Benguerir 43150, Morocco
关键词
Environmental conservation; Agricultural expansion; Tropical watersheds; MapBiomas; CELLULAR-AUTOMATA; SOUTHERN AMAZONIA; CHANGE IMPACTS; CHAIN MODELS; CLIMATE; CERRADO; VEGETATION; ECOSYSTEM; LOCATION; BRAZIL;
D O I
10.1007/s10661-024-12673-4
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Due to the anthropogenic pressures of expansion areas for livestock and agricultural production in the Brazilian Cerrado, it is of paramount importance to understand the dynamics of land use/land cover (LULC) changes in this region. Thus, we investigated LULC changes in two sub-basins of the Tocantins-Araguaia River basin from 1997 to 2015 and consequently projected future changes for the timespan between 2030 and 2050. The Formoso sub-basin experienced significant expansion of agricultural and pasture areas, whereas the Sono sub-basin limited farmland expansion (more stable native vegetation) due to substantial protected areas, trends that were also observed for future projections (2030 and 2050). Pastureland in the Formoso sub-basin increased by 5.8%, while the Sono sub-basin saw significant gains in cultivated land, according to change detection analyses during the 1997-2015 period. High stability probabilities of no change (> 70%) for grassland areas in the Sono River sub-basin and pasturelands in the Formoso River sub-basin were computed. The CA-Markov model demonstrated a high consistency level with actual LULC classes for both sub-basins, as indicated by an overall Kappa coefficient above 0.8. Future projections for 2030 and 2050 show a substantial expansion of agriculture and pasture in both sub-basins, driven by specific factors such as soil organic carbon stocks, distance from rural settlements, and proximity to rivers. Short- and mid-term simulations indicate substantial expansion of agriculture and pasture in both basins, with potential adverse impacts on water erosion. Consequently, developing policies for soil management and sustainable land use planning is essential for agroecosystem sustainability, promoting a balanced approach to economic development while addressing climate change and anthropogenic challenges.
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页数:18
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