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Similarly, the plausibility function for cell c i is, from (4) pl i { A } = 1 − κ · m i ( B ) (14a) pl i { B } = 1 − κ · m i ( A ) (14b).
In Equation 1, the square of absolute deviation from the median is taken to signify the impact of extremes, i.e., the farther the recommendation value x i is from the median, the larger the squared deviation is.
Cvertical(i): The value of i is from 1 to 3. As the RCN of the source node is in the sensory data, M c of the source node can be obtained.
Chorizontal(i): The value of i is from 1 to 3. As the RCN of the source node is in the sensory data, M r of the source node can be obtained.
Where X stands for sieve size and i is from 1 6 (representing the fraction sizes considered for this study), W xi is weight of soil retained on X i, W sxi is weight of sand fraction on X i, W tss is total soil sample, and W st is sand fraction in total soil sample.
According to Eq. (7), the value of d i is from −100nm to +100nm and therefore we can obtain displacement without ambiguity only in a range of 200nm.
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