首页> 外文期刊>Geoderma: An International Journal of Soil Science >Effect of tillage on fractal indices describing soil surface microrelief of a Brazilian Alfisol.
【24h】

Effect of tillage on fractal indices describing soil surface microrelief of a Brazilian Alfisol.

机译:耕作对分形指数的影响,分形指数描述了巴西Alfisol的土壤表面微浮雕。

获取原文
获取原文并翻译 | 示例
           

摘要

Soil surface roughness is known to influence water infiltration, runoff and erosion. Soil surface roughness changes with management and weather and its mathematical description still remains an important issue. The main objective of this study was to investigate the effect of tillage on the two fractal indices, fractal dimension, D, and crossover length, l, currently used in characterizing soil surface microrelief. The statistical index random roughness, RR, was also assessed. Field experiments were done on an Alfisol located at Rio Grande do Sul State (Brazil). Two tillage treatments (conventional versus direct drilling) were tested. The soil surface microrelief was assessed by point elevation measurements in 16 plots for each treatment. The sampling scheme was a square grid with 20x20 mm between point spacing and the plot size was 280x280 mm, so that each data set consisted of 225 individual elevation points. All indices were calculated after trend removal, both by slope correction, i.e., oriented microrelief, and by slope plus tillage marks correction, i.e., random microrelief. The implemented algorithm for estimating D and l consisted in evaluating the roughness around the local root mean square deviation (RMS) of the point elevation values. Irrespective of tillage treatment and detrending procedure, fractal behaviour extended only over a bounded range of scales, from 40 to 100 mm, due to the experimental setup. In these conditions, assessing fractal indices was not always straightforward. The statistical index RR and the fractal index l were significantly different between tillage treatments for oriented and random surface conditions. D values of random soil surfaces were not affected by tillage treatment, whereas D values of oriented microrelief were significantly lower in the direct drilled plots. Removal of tillage marks trend resulted in a significant increase in D values. Within each tillage treatment, l and D were significantly correlated..
机译:已知土壤表面粗糙度会影响水的渗透,径流和侵蚀。土壤表面粗糙度随管理和天气的变化而变化,其数学描述仍然是一个重要的问题。这项研究的主要目的是研究耕作对目前用于表征土壤表面微浮雕的两个分形指数,分形维数D和交叉长度l的影响。还评估了统计指标随机粗糙度RR。现场实验是在南里奥格兰德州(巴西)的Alfisol上进行的。测试了两种耕作处理方式(常规钻井与直接钻井)。通过每次处理的16个样地中的点高测量,评估了土壤表面的微浮雕。采样方案是一个点间距之间为20x20 mm的正方形网格,样区大小为280x280 mm,因此每个数据集由225个单独的高程点组成。所有指数均在趋势消除后通过坡度校正(即定向微浮雕)和坡度加耕marks校正(即随机微浮雕)进行计算。用于估计D和l的已实现算法包括评估点高程值的局部均方根偏差(RMS)周围的粗糙度。不考虑耕种处理和去趋势处理程序,由于实验设置,分形行为仅在40至100 mm的有限范围内扩展。在这种情况下,评估分形​​指数并不总是那么简单。在定向和随机表面条件下的耕作处理之间,统计指数RR和分形指数I显着不同。耕作处理不会影响随机土壤表面的D值,而直接钻孔样地中定向微浮雕的D值则明显较低。去除耕作痕迹的趋势导致D值显着增加。在每次耕作处理中,l和D显着相关。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号