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. 2019 Mar 8;9:3954. doi: 10.1038/s41598-019-40400-4

Table 2.

Correlation relationships between the sediment delivery rate from partially-unfrozen soil slope and that from nonfrozen soil slope.

Slope gradient (°) Flow rate (L/min) Thawed depth (cm) K R 2
10 1 1 1.052 0.994***
2 1.001 0.999***
5 0.907 0.993***
2 1 0.995 0.998***
2 0.899 0.985***
5 0.997 0.998***
4 1 0.861 0.999***
2 0.878 0.999***
5 0.920 0.997***
15 1 1 0.728 0.988***
2 0.870 0.999***
5 0.872 1.0***
2 1 1.014 0.995***
2 0.645 0.991***
5 0.849 0.976***
4 1 0.813 0.997***
2 0.892 0.994***
5 0.888 0.995***
20 1 1 0.748 0.993***
2 0.864 1.0***
5 0.866 0.999***
2 1 0.896 0.994***
2 0.812 0.988***
5 0.903 0.988***
4 1 0.849 0.993***
2 1.029 0.996***
5 0.873 0.996***

Note: K is the ratio of sediment delivery rates between partially-unfrozen soil slope and nonfrozen soil slope; ***Indicates significant at the 0.001 probability level.