SPATIAL VARIATION OF ASH TOTAL CARBON AND TOTAL NITROGEN AFTER A WILDFIRE

被引:0
|
作者
Pereira, Paulo [1 ]
Ubeda, Xavier [2 ]
Martin, Deborah [3 ]
机构
[1] Vilnius Gediminas Tech Univ, Sauletekio Ave 11, LT-10223 Vilnius, Lithuania
[2] Univ Barcelona, Dept Phys Geog & Reg Geog Anal, GRAM Mediterranean Environm Res Grp, Barcelona 08001, Spain
[3] US Geol Survey, Boulder, CO 80303 USA
来源
ENVIRONMENTAL ENGINEERING, VOLS 1-3 | 2011年
关键词
Total Carbon; Total Nitrogen; Wildfire; Fire Severity; Interpolation Methods; Spatial Distribution; INTERPOLATION METHODS; SOIL PROPERTIES; CLIMATE-CHANGE; MANAGEMENT; IRELAND;
D O I
暂无
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The present work aims to study the spatial variability of ash Total Carbon (TC%) and Total Nitrogen (TN%) after a wildfire occurred in Portugal. Ash TC% a mean of 26.72 % (+/- 8.76 %) and ash TN% of 1.20 % (+/- 0.32 %). We observed that the area recover very fast to wildfire and two years the great part of soil was cover by vegetation. The fire severity (assessed with ash color and CaCO3 content) was more related with ash TC%, than ash TN% due the different vulnerability and response of these two elements to fire temperature and as consequence severity. Previous to model data we tested their normality that only was achieved in the case of TC% after a neperian logarithmic transformation (1n). TN% respected gaussian distribution, however showed a high skewness, thus this variable was also In transformed. Ash TC%(1n) presented an excellent spatial structure and the experimental model fits better with the rational quadratic model and ash TN%(1n) with the lineal model. Among all interpolation methods tested, the most accurate to interpolate ash TC%(1n) was IDW2 and the less suitable LP3. In relation to ash TN%(1n) the best interpolation technique was SPT and the less precise LP3. This allow us to observe differences that the spatial distribution of both variables is different, that is due the small scale variability observed in ash TC%(1n). In general the models were well performed because the residuals mean were closed to 0 and no differences between average of predicted and estimated values were identified. Ash TC%(1n) spatial distribution was in higher amounts in western, northern part and southeast and northeast corner of the plot and lower in the centre and south of the interested area and ash TN%(1n) was observed in higher amounts in the southwest and southeast part of the plot and lesser in the central part.
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页码:255 / +
页数:3
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