Aluminum checker plate is widely used in decorative, shipbuilding and architectural applications. Having good forming, drilling and welding ability, Aluminum Diamond Plate is easy to fabricate and its raised diamond lug pattern provides good slip resistance.
Aluminium Propellor Plate is a high shine plate with an embossed pattern resembling an airplane propeller (hence the name). Made in a light soft alloy, it is used for cladding and a wide range of decorative purposes. It is often used for trimming cars, utes and vans because of its highly polished finish. You are able to buy less than full-sized sheets and we can guillotine these to your size (right angle cuts only).
Standard dimensions:
Aluminum checker plate specific applications
Vehicl
Ship
Architecture
Plant
Other
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The corresponding parameters and fractal dimension derived from the theoretical model of average soil moisture variation are derived from the spherical model and the Gaussian model. They fit better to the experimental variogram and the coefficient of determination varies between 0.4 and 0.8, F. The test is extremely significant, indicating that the theoretical variogram model well reflects the spatial structure characteristics of soil moisture. Since the soil moisture shows a base station value for most of the observation period, it shows that the soil moisture has a stable or nearly stationary characteristic in the study area.
Through the measurement of the soil moisture meter, it was found that the degree of spatial variability of soil moisture on the slope surface was inversely proportional to the soil moisture content. When the soil moisture content was low, the degree of spatial variability of the soil moisture was high and the value of the abutment was also high. As the soil moisture content increased The spatial variability of soil moisture decreased, and the value of the abutment also became smaller. The nugget value showed a significant seasonal pattern, which was similar to the average soil moisture content. The soil water base level increases with the soil depth, ie, the soil layer is deepened, and the soil water variability increases. 0) The variability of the 100cm average soil moisture and the profile soil moisture show a fluctuating effect, ie, the experimental semi-variance does not increase monotonically with the increase of the step length, but shows that the similar distance periodically fluctuates up and down to reach the base station value. Later, there are also such fluctuations. This is because the soil moisture is sampled along the slope and the clustering effect of the sample leads to this periodicity. If a uniform grid sampling is established, this phenomenon will be reduced. The periodicity may be related to the terrain and geomorphology factors in the study area, or it may be related to artificial soil preparation. Under the scale of this study, the micro-geomorphic pattern on the slope is the main reason.
thickness 1.6&1.8 mm, width and length can be customized cut to suit size.
Applications: checker plate floor, such as van-type vehicle catwalk flooring, wood step of the bus or truck, train inspection hole lid, tank car, the car cold storage.
Applications: corridor and bridges over the lid and floors, stairs, cabin deck, fish tank, gangway to the floating dock.
Applications: floors, stairs, shelves, such as gutter lid, the bicycle.
Applications: bench floor and stairs, equipment/ plant machinery, such as ambulatory inspection.
Applications: such as a deck ladder, ladder, showcase, temporary scaffolding, the structure of marine.
Soil Moisture Analyzer Used to Analyze the Temporal and Spatial Distribution of Soil Moisture in Loess Region
The soil is a continuum of temporal and spatial variation. There are obvious differences in soil characteristics in different spatial locations, ie the spatial variability of soil properties. In order to describe the spatial variability of soil moisture, the traditional soil survey is to divide the soil into several relatively uniform areas on the plane according to the texture of the soil. In the depth, it is divided into different soil layers to describe the spatial variability of the soil. This is basically a qualitative description method, rather than a quantitative estimate. In many cases, it is difficult to accurately describe the spatial distribution of soil traits (such as soil moisture). When studying a soil characteristic, first understand the study area. The background conditions are very necessary and are the basis for further research. Soil moisture meter can effectively determine the soil moisture content.