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Water productivity of different land uses in watersheds assessed from satellite imagery Landsat 5 Thematic Mapper.

机译:根据卫星图像Landsat 5 Thematic Mapper评估的流域内不同土地利用的水生产率。

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摘要

Water productivity (WP) of various classes of soil usage from watersheds was estimated using the SAFER - Simple Algorithm For Evapotranspiration Retrieving - algorithm and the Monteith equation to estimate the parameters of biomass production (BIO). Monteith?s equation is used to quantify the absorbed photosynthetically active radiation (APAR) and Actual Evapotranspiration (ET) was estimated with the SAFER algorithm. The objective of the research is to analyze the spatial-temporal water productivity in watersheds with different uses and soil occupation during the period from 1996 to 2010, in conditions of drought and using the Monteith model to estimate the production of BIO and using the SAFER model for ET. Results indicated an increase of 153.2% in ET value during the period 1997-2010, showing that the irrigated areas were responsible for this increase in ET values. In September 2000, image of day of year (DOY) 210 showed high values of BIO, with averages of 80.67 kg ha-1d-1. In the year 2010 (DOY:177), the mean value of BIO was 62.90 kg ha-1d-1, with an irrigated area with a maximum value of 227.5 kg ha-1d-1. The highest incremental values of BIO is verified from the start of irrigated areas equal to the value of ET, because there is a relationship between BIO and ET. The maximum water productivity (WP) value occurred in June/2001, with 3,08 kg m-3, the second highest value was in 2010 (DOY:177), with a value of 2,97 kg m-3. Irrigated agriculture show the highest WP value, with maximum value of 6.7 kg m-3. The lowest WP was obtained for DOY 267, because of the dry season with condition of low soil moisture.
机译:使用SAFER-蒸散检索简单算法-算法和Monteith方程估算流域各种类型土壤利用的水生产率(WP),以估算生物量生产(BIO)的参数。蒙特斯方程用于量化吸收的光合有效辐射(APAR),并使用SAFER算法估算实际蒸散量(ET)。本研究的目的是分析干旱条件下1996年至2010年不同用途和土壤占用的流域的时空水分生产率,并使用Monteith模型估算BIO的产生,并使用SAFER模型对于ET。结果表明,在1997年至2010年期间,ET值增加了153.2%,这表明灌溉区域是ET值增加的原因。 2000年9月,年度(DOY)210图像显示了较高的BIO值,平均值为80.67 kg ha-1d-1。在2010年(DOY:177),BIO的平均值为62.90 kg ha-1d-1,灌溉面积的最大值为227.5 kg ha-1d-1。从BIO和ET之间存在关系开始,从灌溉区域开始就验证了BIO的最高增量值等于ET的值。最大水生产率(WP)值发生在2001年6月,为3,08 kg m-3,第二高的是2010年(DOY:177),为2,97 kg m-3。灌溉农业的WP值最高,最大值为6.7 kg m-3。由于干旱季节和土壤湿度低的条件,DOY 267的WP最低。

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