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9 Reference List: What Is The Measuring Wheel Used For With Erosion Control | Dictionary Geotechnical Engineering / Wörterbuch GeoTechnik: Volume I …
- A simple method for measuring the sediment concentration is to store all runoff or to divide it using a sequence of tanks. In each tank the mean concentration Cm (g/L) is estimated from the concentration profile obtained by collecting samples of given volume at different depths. If Cm is calculated by integrating the concentration profile measured along the axial vertical of a tank wall, Bagarello and Ferro [6Q] illustrated that the actual concentration C (g/L) is linked to Cm according to the following relationship: - Source: Internet
- Figure 4.21. Layout of an experimental plot for soil erosion studies. Source: [29]. - Source: Internet
- In many laboratory and plot studies, a rainfall simulator is used to reproduce a storm of known kinetic energy and drop-size distribution. Rainfall simulators are ideal tools for distinguishing the effects of single factors on soil erosion and for carrying out a large number of experimental runs in a short time. Desired characteristics of rainfall simulators [66, 67] include a wide range of intensities, drop sizes, fall velocities, and impact energy characteristics similar to those of natural rainstorms; uniformity of spray pattern and of drop-size distribution on the plot area; and continuous application of rain or minimum time between simulated raindrop applications if intermittent. - Source: Internet
- Studies on sheet erosion due to overland flow need small plot width (2-3 m) and length (<10 m). Studies on rill erosion require plot lengths greater than 6-13 m [29]. Sites should be selected to represent the range of uniform slopes prevailing in the farming area under consideration. Slopes ranging from convex to concave are used to evaluate the influence of the slope shape on soil loss. Because the plot area is known, soil loss can be expressed as kg/m2 per unit time, which assumes a uniform soil loss over the plot. - Source: Internet
- Where soil erosion has occurred, 137Cs also will have been lost, leading to a reduced loading. Conversely, where soil deposition takes place, an increase in 137Cs activity will be found. The geostatistical analysis of local 137Cs activity measurements allows establishment of the spatial distribution of the 137Cs percentage residuals Y = (137Cs — Csrif)/Csrif which is correlated with the mean annual sediment yield spatial distribution [4, 65]. - Source: Internet
- There are many points to understand about To take the most accurate reading from a wheel, you first need to dedicate the appropriate amount of time and energy to understanding how your tool works. Read the manual, research tips on the internet, and see what you can accomplish.There are many points to understand about measuring wheels . Take time to learn more about the options available to you at Engineer Supply and get the best tools for your next job. - Source: Internet
- Whether you work as a contractor, a surveyor, or a home remodeler, one of the most important tasks you are responsible for is taking an accurate measurement of the land. Such readings are crucial before you can conduct any actual work. Naturally, you want to make sure you have all of the right tools and gear to help you complete your job. When you need to guarantee accurate readings, measuring wheels are some of the best options available to you. - Source: Internet
- In an experimental station for soil erosion studies, bounded runoff plots of known width, slope length, slope steepness, and soil type are monitored. Plot size depends on the physical process under investigation. Early basic data used for the development of the Universal Soil Loss Equation (USLE) [57] were often obtained from plots 40.5 m2 in size, having a standard length of 22.1 m [54]. - Source: Internet
- For a steep-slope channel, the discharge of the uniform flow is calculated by the Chezy’s law, measuring the flow depth. In this case, the channel length has to be calculated to avoid the roll-wave formation [63]. The flow-depth measurement can be obtained by a nonintrusive, ultrasonic-level probe. The probe sends an ultrasonic pulse that, after partial reflection, is detected by the same sensor and converted back into an electrical signal. The time between transmission and reception of the pulse is directly proportional to the distance between the probe and the water surface. - Source: Internet
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