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Calibration points' data are then acquired by using a two-axis rotary table and a star simulator.
Then, (frac {{{mathrm {1 - }}alpha }}{alpha }N) points data are removed at the end.
Where outcomes are reported for multiple time points, data are presented for each time point.
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Typical GPS track points data is a serious of sequential track points.
After the DFT processing, a (frac {N}{alpha }) points data is acquired.
At all the three time points, data were scattered over a large range of TBF values.
After DFT processing, a (frac {N}{alpha }) points data is acquired.
After IDFT processing, a (frac {N}{alpha }) points data is acquired.
Since melting point data are difficult to obtain without making the actual salt, predicting salt solubility remains difficult.
For regional soil studies where polygon mapping and soil point data are available, ensemble modelling is a useful combinatorial approach.
The freeze point data are provided in Table 1.
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