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71.
72.
异龄林既是一个自然生态系统,又是一个复杂的森林经营系统。一个经营工作者要对异龄林进行高效率的经营,就必须掌握现实林的动态变化规律,以便有目的地制定经营措施。异龄林系统从经营角度出发,可以划分成如下三个组成单元:进界生长量、向上生长量和枯损量。上述三个单元的相互作用构成了异龄林系统的动态变化规律。本文的主要目的就是通过对上述三个生长单元的动态进行模拟,寻找出异龄林的动态变化规律,所用方法是对每个生长单元用多个数学模型进行拟合,再通过统计量分析和实际验证从中选出最理想的模型,并据此对现实异龄林的动态进行预测。证明了以曲线形式反映异龄林的动态变化远优于线性形式。所用材料取自黑龙江省小兴安岭和牡丹江林区的冷杉(Abies nephrolepis)为主的异龄针阔混交林。 相似文献
73.
74.
膨化机三维参数化设计系统的研究 总被引:1,自引:0,他引:1
详细介绍了基于机械自动化设计软件Solidworks研制的膨化机三维参数化设计系统的功能结构、人机界面和关键技术的处理方法。该系统完全被封装在Solidworks的一个菜单项下,通过简单的人机交互,输入功率、转速等设计参数后,它就能自动完成整台膨化机的结构设计,包括膨化腔、带轮传动和减速箱传动的全部设计过程,具有一定的智能化,然后根据用户选择输出零件或者装配体的三维实体模型和工程图。零件自动三维造型的实现采用了以尺寸驱动为主,程序驱动为辅的编程思想,并建立相应的膨化机模板零件库。整个系统程序使用VisualC 语言开发,以动态链接库的形式嵌入Solidworks系统,实现了与Solidworks软件的无缝结合。配合Solidworks强大的三维造型、设计和装配功能,极大地提高了膨化机设计的效率、精度和质量。 相似文献
75.
熊渊博 《湖南农业大学学报(自然科学版)》2003,30(2)
提出了一种ARMA模型的线性估计方法,这种方法通过两次AR模型的估计来实现ARMA的估计。讨论了一维时间序列开环系统、闭环系统的辨识方法及定阶问题。仿真结果表明该方法具有良好的准确度和可靠性,可直接用于结构状态监测。 相似文献
76.
异龄林既是一个自然生态系统,又是一个复杂的森林经营系统。一个经营工作者要对异龄林进行高效率的经营,就必须掌握现实林的动态变化规律,以便有目的地制定经营措施。异龄林系统从经营角度出发,可以划分成如下三个组成单元:进界生长量、向上生长量和枯损量。上述三个单元的相互作用构成了异龄林系统的动态变化规律。本文的主要目的就是通过对上述三个生长单元的动态进行模拟,寻找出异龄林的动态变化规律,所用方法是对每个生长单元用多个数学模型进行拟合,再通过统计量分析和实际验证从中选出最理想的模型,并据此对现实异龄林的动态进行预测。证明了以曲线形式反映异龄林的动态变化远优于线性形式。所用材料取自黑龙江省小兴安岭和牡丹江林区的冷杉(Abies nephrolepis)为主的异龄针阔混交林。 相似文献
77.
The effect of tillage direction on soil redistribution by mouldboard ploughing on complex slopes 总被引:1,自引:0,他引:1
Seven mouldboard ploughing experiments were conducted to systematically investigate the effect of different tillage directions on soil redistribution on hillslopes. The present study included tillage directions other than parallel to the gradient or along the contour, that is, in our experiments the slope gradient changed simultaneously in tillage and in turning direction. Using physical tracers we developed a model of the two-dimensional tracer displacement as a function of topography and tillage variables. The displacements in tillage and in turning direction were separately described as 2nd degree polynomials in both tillage and in turning directions. This model fully accounted for the directionality of tillage. Displacement in turning direction additionally depended on tillage depth, while that in tillage direction was affected by tillage speed and soil bulk density. We found a large effect of tillage directionality on soil redistribution, and tillage at 45° to the gradient turning soil upslope was the least erosive tillage direction. We obtained non-linear relationships between soil redistribution and profile curvature, instead of the linear relationships reported previously. Consequently tillage erosivity varied in tillage direction and a unique tillage transport coefficient could not be obtained for all tillage directions. 相似文献
78.
Modelling of snowmelt erosion and sediment yield in a small low-mountain catchment in Germany 总被引:1,自引:0,他引:1
Temporal variability and spatial heterogeneity of surface runoff generation triggers the dynamics of source areas of sediment and sediment-associated nutrient transport. Reliable modelling of hydrological special situations i.e. snowmelt is of high importance for the quality of erosion and sediment yield modelling. Data from the research catchment Schäfertal demonstrate the individuality of snowmelt events in terms of runoff coefficient and delivery ratio. This 1.44 km2 low mountain catchment is characterised by a high portion of arable land with a winter grain/winter rape crop rotation. The integrated winter erosion and nutrient load model (IWAN) considers these dynamic aspects by coupling a hydrological model with a sediment load model. Cell size of this raster-based approach is 10 × 10 m2. Additionally, snowmelt rill erosion is simulated with a newly developed physically based model that is firstly applied on a catchment scale. A sensitivity analysis of this model system component demonstrates the plausibility of the model approach and the overall robustness of the model system IWAN. The results of the long-term hydrological modelling from 1991 to 2003 are reliable and form the basis for the simulation of six snowmelt events which were observed in the Schäfertal catchment. The estimated total runoff volumes for these events match the observations well. The modelled overland runoff coefficients vary from 0.001 to 0.72. The mean values of cell erosion, which were modelled with one set of parameters for all six events range from 0.0006 to 0.96 t ha− 1. The total modelled erosion for the events with unfrozen soil and low amount of surface runoff is of a factor 50 below those with partly frozen soil. In addition to these distinctions, the major differences are caused by flow accumulation in shallow depressions in variable parts of the catchment. However, the validation of these results on the single event scale is restricted due to limited spatial data. Total simulated sediment yield at the catchment outlet was as high as 13.84 t which underestimates the observed values, with the exception of one event. Oversimplification of the modelled channel processes may be a reason. The temporal variability and spatial heterogeneity of the surface roughness parameter, which was identified to be sensitive, also causes uncertainty in the parameter estimation. Despite these findings, the model system IWAN was applied successfully on the catchment scale and the simulated results are reliable. 相似文献
79.
R. P. C. Morgan 《CATENA》2001,44(4)
A revised version of the Morgan–Morgan–Finney model for prediction of annual soil loss by water is presented. Changes have been made to the way soil particle detachment by raindrop impact is simulated, which now takes account of plant canopy height and leaf drainage, and a component has been added for soil particle detachment by flow. When tested against the same data set used to validate the original version at the erosion plot scale, predictions made with the revised model gave slopes of a reduced major-axis regression line closer to 1.0 when compared with measured values. The coefficient of efficiency, for sites with measured runoff and soil loss, increased from 0.54 to 0.65. When applied to a new data set for erosion plots in Denmark, Spain, Greece and Nepal, very high coefficients of efficiency of 0.94 for runoff and 0.84 for soil loss were obtained. The revised version was applied to two small catchments by dividing them into land elements and routing annual runoff and sediment production over the land surface from one element to another. The results indicate that, when used in this way, the model provides useful information on the source areas of sediment, sediment delivery to streams and annual sediment yield. 相似文献
80.