巴西塞拉多源头Córrego da Formiga土地利用与水质联合动态

Q3 Social Sciences
P. R. Giongo, Ana Paula Aparecida de Oliveira Assis, M. Silva, A. Montenegro, J. Taveira, Adriana R Costa, P. C. Silva, A. M. M. Giongo, Héliton Pandorfi, Alessandro José Marques Santos, C. Backes, Maria Beatriz Ferreira, J. L. B. D. Silva
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引用次数: 0

摘要

巴西塞拉多生物群落为巴西和南美洲提供了相关的生态系统服务,对水资源的规划和管理以及农业综合企业具有战略意义。目的是评价巴西塞拉多(Cerrado)未开发地区Córrego da Formiga河沿岸的水质、土地利用与水的物理化学和生物参数的关系以及支流的流入情况。2015年确定了5个取水点(在水源和河口之间),并按季度进行观测,在实验室采集水样并分析其物理化学和生物参数,并在取水的同一点和当天进行流量测量。为了识别和量化流域的土地利用和土地覆盖(LULC),利用Landsat8-OLI卫星图像和其他地貌数据(Topodata-INPE)生成每个集水点的坡度、流域划界和贡献面积。各集水点贡献区域的LULC百分比与水的物理化学和生物参数相关,并提交多变量分析(PLS-DA)对五个分析点进行分析和分组。在进行第一次和最后一次采样的时间(雨季),水质模式的变化更为明显,并可能受到这些时期水量增加的影响。水流随时间和点间变化很大,最低记录流量为0.1 L s−1 (P1),最高记录流量为947.80 L s−1 (P5)。Córrego da Formiga的水质为III级(CONAMA决议357),其特点是对多种用途的用水限制很小。原生植被覆盖面积略高于12%,以甘蔗类(62.42%)和牧草类(19.33%)为主。PLS-DA分析允许在P1、P2、P3和P5之间分离水分析点,而P4则叠加在其他点上。还可以验证,对这种水质分离最重要的参数是pH、碱度t、碱度h、钙和硬度,它们都有从源头(P1)到口(P5)浓度增加的趋势。在水质方面,也可以验证P2点和P5点的水质条件较好。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Land Use and Water-Quality Joint Dynamics of the Córrego da Formiga, Brazilian Cerrado Headwaters
The Brazilian Cerrado biome provides relevant ecosystem services for Brazil and South America, being strategic for the planning and management of water resources as well as for agribusiness. The objective was to evaluate the water quality along the course of the Córrego da Formiga in a virgin portion of the Brazilian Cerrado, the relationship of land use with physical-chemical and biological parameters of the water, and the inflow of the tributary. Five water collection points were defined (between the source and mouth) and observed on a quarterly scale in 2015, water samples were collected and analyzed for physical-chemical and biological parameters in the laboratory, and flow measurements were performed at the same point and day of water collection. To identify and quantify land use and land cover (LULC) in the watershed, an image from the Landsat8-OLI satellite was obtained, and other geomorphological data from hypsometry (Topodata-INPE) were obtained to generate the slope, basin delimitation, and contribution area for each water collection point. The LULC percentages for each area of contribution to the water collection points were correlated with the physical-chemical and biological parameters of the water and submitted to multivariate analysis (PLS-DA) for analysis and grouping among the five analyzed points. Changes in water-quality patterns were more pronounced concerning the time when the first and last sampling was performed (rainy period) and may be influenced by the increase in the volume of water in these periods. The stream flow is highly variable over time and between points, with the lowest recorded flow being 0.1 L s−1 (P1) and the highest being 947.80 L s−1 (P5). Córrego da Formiga has class III water quality (CONAMA resolution 357), which characterizes small restrictions on the use of water for multiple uses. The soil cover with native vegetation is just over 12%, while the predominance was of the classes of sugar cane (62.42%) and pasture (19.33%). The PLS-DA analysis allowed separating the water analysis points between P1, P2, P3, and P5, while P4 was superimposed on others. It was also possible to verify that the parameters that weighed the most for this separation of water quality were pH, alkalinity_T, alkalinity_h, calcium, and hardness, all with a tendency to increase concentration from the source (P1) to the mouth (P5). As for water quality, it was also possible to verify that points P2 and P5 presented better water-quality conditions.
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来源期刊
Human Geographies
Human Geographies Social Sciences-Geography, Planning and Development
CiteScore
1.10
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