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Table 2 XRF data of the SG12LM3 samples and suspended material from the Hasu River

From: Mass accumulation rate of detrital materials in Lake Suigetsu as a potential proxy for heavy precipitation: a comparison of the observational precipitation and sedimentary record

  Distance from the core top (cm) XRF data (wt%)   
SG12LM3 Top Bottom LOI SiO2 TiO2 Al2O3 Fe2O3 MnO MgO CaO Na2O K2O P2O5 C det(wt%) DBD(g/cm3)
SG12LM3-02 0.5 1.1 33.40 62.09 0.77 16.45 7.74 0.10 3.15 1.02 4.49 3.54 0.63 41.78 0.12
SG12LM3-03 1.1 1.7 35.93 60.46 0.72 16.27 8.85 0.17 3.16 1.01 5.04 3.74 0.58 38.83 0.11
SG12LM3-04 1.7 2.2 28.14 59.41 0.84 17.60 9.64 0.21 3.13 0.92 4.56 3.29 0.40 47.28 0.13
SG12LM3-05 2.2 2.8 27.97 61.60 0.81 17.27 8.18 0.21 2.99 0.91 4.44 3.17 0.42 47.63 0.14
SG12LM3-06 2.8 3.4 27.67 56.96 0.77 18.93 10.50 0.23 3.02 0.91 5.28 3.03 0.38 50.43 0.13
SG12LM3-07 3.4 4 24.01 56.06 0.90 21.51 9.57 0.26 2.96 0.83 4.35 3.18 0.37 61.53 0.16
SG12LM3-08 4 4.6 34.20 57.54 0.83 17.83 9.02 0.23 3.53 1.30 5.28 4.02 0.41 42.93 0.11
SG12LM3-09 4.6 5.2 29.43 60.21 0.79 17.22 9.07 0.23 3.02 1.01 4.80 3.28 0.38 45.66 0.14
SG12LM3-10 5.2 5.8 26.25 58.81 0.80 17.39 10.32 0.23 3.06 0.91 5.11 3.05 0.32 47.43 0.15
SG12LM3-11 5.8 6.4 22.63 59.57 0.86 19.00 9.43 0.21 3.00 0.79 3.93 2.94 0.27 56.08 0.18
SG12LM3-12 6.4 7 26.25 60.46 0.80 17.83 8.27 0.23 3.02 0.87 4.94 3.27 0.30 49.98 0.16
SG12LM3-13 7 7.6 27.91 57.97 0.81 17.87 10.54 0.30 3.01 0.91 4.87 3.38 0.33 47.43 0.13
SG12LM3-14 7.6 8.2 28.25 56.94 0.80 17.28 10.64 0.33 3.16 1.19 5.75 3.61 0.31 44.66 0.13
SG12LM3-15 8.2 8.9 24.33 59.39 0.84 18.13 9.25 0.32 2.94 0.86 4.61 3.37 0.29 51.64 0.13
SG12LM3-16 8.9 9.5 24.61 57.85 0.87 18.01 10.64 0.36 3.05 0.94 4.90 3.10 0.28 49.99 0.15
SG12LM3-17 9.5 10.1 28.22 56.25 0.88 17.84 10.89 0.37 3.14 1.05 5.77 3.46 0.36 46.06 0.14
SG12LM3-18 10.1 10.7 24.45 56.37 0.88 19.38 10.90 0.39 2.95 0.83 4.62 3.36 0.32 53.82 0.16
SG12LM3-19 10.7 11.3 21.70 55.61 0.95 19.98 11.31 0.39 3.08 1.02 4.29 3.05 0.31 57.43 0.19
SG12LM3-20 11.3 11.9 22.66 56.21 0.95 19.08 11.57 0.40 3.14 0.97 4.45 2.94 0.29 53.94 0.17
SG12LM3-21 11.9 12.55 20.54 57.57 0.98 19.23 11.35 0.39 3.04 0.81 3.47 2.83 0.33 56.95 0.20
SG12LM3-22 12.55 13.1 17.01 55.66 1.05 21.39 11.28 0.35 3.13 0.74 3.34 2.77 0.29 66.41 0.23
SG12LM3-23 13.1 13.7 17.96 55.37 1.02 21.47 11.37 0.36 3.10 0.79 3.42 2.80 0.31 65.70 0.24
SG12LM3-24 13.7 14.3 20.40 56.80 1.00 19.20 11.84 0.50 3.19 0.82 3.60 2.79 0.26 56.39 0.21
SG12LM3-25 14.3 14.95 20.36 56.31 1.00 19.37 11.92 0.57 3.17 0.82 3.74 2.83 0.27 56.66 0.21
SG12LM3-26 14.95 15.55 23.79 56.72 0.93 18.96 11.44 0.65 3.07 0.91 4.00 3.03 0.30 53.07 0.20
SG12LM3-27 15.55 16.2 19.77 54.14 1.01 21.63 12.26 0.65 3.00 0.74 3.34 2.93 0.31 63.82 0.22
SG12LM3-28 16.2 16.7 25.15 55.31 0.93 19.15 12.61 0.74 3.02 0.88 4.06 2.96 0.35 51.80 0.19
SG12LM3-29 16.7 17.3 26.46 54.52 0.88 17.91 14.33 0.76 2.96 0.95 4.31 3.03 0.36 46.30 0.18
SG12LM3-30 17.3 17.9 27.41 55.49 0.89 17.99 13.01 0.69 3.02 1.12 4.24 3.04 0.49 46.59 0.18
SG12LM3-31 17.9 18.55 27.45 55.36 0.89 17.88 13.49 0.64 3.02 0.91 4.58 2.88 0.35 46.13 0.17
SG12LM3-32 18.55 19.2 28.59 53.72 0.86 17.57 14.68 0.64 3.03 0.88 5.05 3.22 0.35 43.42 0.17
SG12LM3-33 19.2 19.75 28.11 55.15 0.88 17.69 14.22 0.60 2.95 0.88 4.35 2.94 0.34 44.96 0.18
SG12LM3-34 19.75 20.4 25.61 57.31 0.89 17.69 12.96 0.47 2.85 0.80 4.05 2.66 0.33 47.92 0.19
SG12LM3-35 20.4 21 24.26 63.60 0.77 15.40 10.54 0.34 2.48 0.66 3.56 2.36 0.28 44.72 0.20
SG12LM3-36 21 21.6 21.17 67.21 0.71 14.10 9.14 0.27 2.26 0.58 3.29 2.20 0.24 43.89 0.21
SG12LM3-37 21.6 22.2 19.12 67.91 0.67 13.23 9.58 0.25 2.17 0.57 3.44 1.95 0.24 42.14 0.22
SG12LM3-38 22.2 22.7 21.99 67.29 0.67 13.33 9.68 0.24 2.16 0.58 3.42 2.38 0.25 40.70 0.22
SG12LM3-39 22.7 23.3 21.60 56.03 0.91 18.25 13.17 0.52 3.00 0.83 4.15 2.84 0.31 51.60 0.20
SG12LM3-40 23.3 23.9 21.16 63.84 0.78 15.43 10.37 0.30 2.45 0.65 3.44 2.48 0.27 46.80 0.21
SG12LM3-41 23.9 24.5 21.63 65.43 0.73 14.29 10.22 0.28 2.32 0.62 3.51 2.34 0.26 43.34 0.22
Hasu River                
SG121001-01 16.20 53.53 1.55 20.61 13.41 0.53 3.98 1.83 1.62 2.33 0.60