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Fire effects on soil water dynamics in a Mediterranean shrubland

机译:地中海灌木丛中土壤水动态的火灾作用

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With the purpose of studying the effects of fire on the natural dynamics of soil water, an experiment was set in a Mediterranean shrubland in Central West Portugal. Soil moisture was measured in two closely located plots at six depths down to 170 cm, during 2000 (reference period) and after an experimental fire set on one of the plots in June 2001 (treatment period). Moisture differences between homologous days (I) of the treatment and the reference periods were computed both for the control (Dci) and for the burned (Dbi) plots. Results showed significantly higher values of Dbi both at the dry and at the rainy seasons. Values of Dci were subtracted from Dbi in order to estimate the net effect of fire on soil water storage (Si). Values of Si showed a maximum of 108.2 mm in the dry season and a maximum of 145.2 mm in the rainy season. At the upper soil layers values of Si decreased as vegetation recovery proceeded along the dry season.
机译:目的是研究火灾对土壤水域自然动态的影响,在中西部葡萄牙的地中海灌木丛中设有实验。在2000年(参考时期)和2001年6月的一个地块(治疗期)的实验火灾中,在六个深度为170厘米的六个深度,在六个深入的位置测量土壤水分。对照(DCI)和烧伤(DBI)图来计算治疗的同源天(I)之间的湿气差异和参考时段。结果表明,在干燥和雨季,DBI的值显着更高。从DBI中减去DCI的值,以估计火灾对土壤储水(SI)的净效应。旱季的Si值最高显示最多108.2毫米,雨季最多可达145.2毫米。随着养殖恢复沿着干燥季节进行,Si的上层分层减少。

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