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Crop residue in North Dakota: measured and simulated by the wind erosion prediction system.

机译:北达科他州的农作物残留:通过风蚀预测系统进行测量和模拟。

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摘要

Residue cover is very important for controlling soil erosion by water and wind. Thus, the wind erosion prediction system (WEPS) includes a model for the decomposition of crop residue. It simulates the fall rate of standing residue and the decomposition of standing and flat residue as a function of temperature and moisture. It also calculates residue cover from flat residue mass. Most of the data used to develop and parameterize this model have been collected in the southern USA. We compared WEPS-simulated residue cover with that measured in south-central North Dakota for 50 two-year cropping sequences from nine crops species that were grown using no-till management. Measured data included residue mass at the time of harvest and residue cover just after seeding the next spring. Simulated residue cover significantly (P<0.05) underestimated measured cover for 33 out of the 50 simulated cropping sequences and overestimated measured cover for five cropping sequences. Some of the differences may be explained by the fact that, for many WEPS crops, residue decomposition parameters are not based on measured field data, but on expert judgment. In addition, WEPS did not predict any stem fall for most of the crops during winter, which contradicts observations that storms flatten many residue stalks of crops such as sunflower. In addition to stem fall and residue decay by biological means, which are driven by temperature and moisture, the model needs to explicitly simulate stem fall by mechanical forces, such as wind- and snowstorms, which are important in northern climates. Furthermore, WEPS does not model the migration of unanchored residue caused by rain- or windstorms, although this does affect residue mass-to-cover ratios and susceptibility to erosion. This study will help improve the WEPS decomposition model and its parameterization, but more data on residue decay and stem fall are needed for different climates and crops to ensure the applicability of the model over a wide range of conditions.
机译:残留物覆盖对于控制水和风对土壤的侵蚀非常重要。因此,风蚀预测系统(WEPS)包括用于分解农作物残渣的模型。它模拟了残留物的下降速度以及残留物和平坦残留物的分解随温度和湿度的变化。它还可以根据残留残渣的质量计算残渣覆盖率。用于开发和参数化此模型的大多数数据已在美国南部收集。我们将WEPS模拟的残留覆盖率与北达科他州中南部测得的9种作物的50种两年种植序列的残留覆盖率进行了比较,这些作物使用免耕管理种植。测得的数据包括收获时的残留物质量和第二年春季播种后的残留物覆盖率。 50个模拟耕作序列中的33个的模拟残留量覆盖率显着(P <0.05)低估了耕作覆盖率,五个耕种序列的模拟量残留量覆盖率高估了。对于许多WEPS作物而言,残留物分解参数不是基于实测田间数据,而是基于专家判断的事实,可以解释某些差异。此外,WEPS并未预测大多数农作物在冬季会掉落,这与暴风雨使向日葵等农作物的许多残留茎变平的观察结果相矛盾。除了通过温度和湿度驱动的生物手段使茎倒下和残留物腐烂之外,该模型还需要通过机械力(例如在北部气候中非常重要的风和暴风雪)明确模拟茎倒下。此外,WEPS并未对由暴风雨或暴风雨引起的未锚定残留物的迁移进行建模,尽管这确实影响了残留物的质量/覆盖比和易腐蚀性。这项研究将有助于改善WEPS分解模型及其参数化,但是对于不同的气候和农作物,还需要更多有关残留物腐烂和茎倒下的数据,以确保该模型在各种条件下的适用性。

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