首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Measurement and simulation of wind erosion, roughness degradation and residue decomposition on an agricultural field
【24h】

Measurement and simulation of wind erosion, roughness degradation and residue decomposition on an agricultural field

机译:农田风蚀,粗糙度降低和残留物分解的测量和模拟

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

The Wind Erosion Prediction System (WEPS) includes submodels to simulate soil erosion by wind, roughness degradation and residue decomposition. These WEPS submodels were tested using data measured on a 600 m to by 415 m farmer's field, planted with winter wheat, near Burlington, Colorado, USA. Big Spring Number Eight (BSNE) samplers were used to measure wind blown sediment flux and automated devices (Sensits) detected saltating sediment. A weather station recorded relevant meteorological data. Detailed measurements of field surface conditions were taken on three dates. One significant dust storm occurred during the experimental period (November 2000 to April 2001). Spatial variability of sediment discharge was high. This could partially be explained by spatial differences in residue cover and mass, leaf area index, sand fraction and wetness of the surface soil. WEPS overestimated the ability of small wheat plants to protect the soil against wind erosion. A simulation without any wheat plants produced a large field sediment loss of 4.43 kg m~(-2), whereas a simulation with very small wheat plants (height = 10 mm, leaf area index = 0. 1, stem area index = 0.01) produced no erosion. This component of WEPS is based on laboratory wind tunnel experiments with simulated standing biomass uniformly spaced on a flat surface. Wheat biomass in the field is not uniformly spaced. WEPS should be modified to account for these non-uniform realities. Mean ridge height was reduced from 42 min on 19 December to 34 mm (36 mm simulated using WEPS) on 12 April. Mean random roughness was reduced from 5.8 min on 19 December to 5.2 mm (5.3 mm simulated) on 8 March. Mean corn residue biomass was reduced only slightly from 1204 kg ha~(-1) on 19 December to 1174 kg ha~(-1) (1075-1175 kg ha~(-1) simulated) on 12 April. These differences between measured data and simulations were not significant (P > 0.05), enhancing confidence in the ability of WEPS to simulate roughness degradation and residue decomposition.
机译:风蚀预测系统(WEPS)包含子模型,可模拟风,粗糙度降低和残留物分解对土壤的侵蚀。使用在美国科罗拉多州伯灵顿附近种植冬小麦的600 m至415 m农民田间测量的数据对这些WEPS子模型进行了测试。八号大泉(BSNE)采样器用于测量风吹沉积物通量,自动装置(Sensits)检测盐分沉积物。一个气象站记录了相关的气象数据。在三个日期对田间地面条件进行了详细的测量。在实验期间(2000年11月至2001年4月)发生了一场重大沙尘暴。泥沙排放的空间变异性高。这部分可以通过残留物覆盖和质量,叶面积指数,沙分和表层土壤湿度的空间差异来解释。 WEPS高估了小型小麦植物保护土壤免受风蚀的能力。没有任何小麦植株的模拟产生了4.43 kg m〜(-2)的大田沉积物损失,而具有非常小的小麦植株的模拟(高度= 10 mm,叶面积指数=0。1,茎面积指数= 0.01)没有产生侵蚀。 WEPS的这一部分基于实验室风洞实验,模拟的固定生物量均匀地分布在平坦表面上。田间的小麦生物量分布不均匀。应修改WEPS以解决这些不一致的现实。平均脊高从12月19日的42分钟降低到4月12日的34毫米(使用WEPS模拟的36毫米)。平均随机粗糙度从12月19日的5.8分钟减少到3月8日的5.2毫米(模拟的5.3毫米)。平均玉米残留生物量仅略有减少,从12月19日的1204 kg ha〜(-1)降至4月12日的1174 kg ha〜(-1)(模拟量为1075-1175 kg ha〜(-1))。测量数据与模拟之间的这些差异并不显着(P> 0.05),从而增强了人们对WEPS模拟粗糙度降低和残渣分解的能力的信心。

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