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. 2022 Feb 2;158(1):39–72. doi: 10.1007/s10533-021-00884-7

Table 6.

Results of isotopic exchange analyses for the study sites Mangfallgebirge, Tuttlingen, Schänis, and Bärenthal (mean ± standard deviation, n = 3). Water extractable P (Pw) and total inorganic P (Pi). Fitting parameters (m and n) describing the decrease of radioactivity in the solution with time, amount of P isotopically exchangeable within 1 min (E1min), between 1 min and 1 day (E1min-1 day), between 1 day and 3 months (E1day-3 months), and amount of P not exchangeable within 3 months (E>3 months)

Pw
(µg P g−1 soil)
Pi
(µg P g−1 soil)
m N E1min
( µg P g−1 soil)
E1min-1 day
( µg P g−1 soil)
E1day-3 months
( µg P g−1 soil)
E> 3 months
( µg P g−1 soil)
Mangfallgebirge S1
Ah1 2.97 ± 0.86 134.6 0.51 ± 0.18 0.59 ± 0.03 7.5 ± 4.5 93.4 ± 11.6 30.4 ± 14.1 3.3 ± 1.9
Bk 0.19 ± 0.21 48.2 0.03 ± 0.01 0.59 ± 0.10 5.2 ± 4.5 33.8 ± 4.7 8.0 ± 7.0 1.2 ± 1.4
Mangfallgebirge S2
Ah 0.66 ± 0.29 138.9 0.17 ± 0.06 0.61 ± 0.07 4.4 ± 2.6 92.3 ± 14.5 37.9 ± 13.2 4.3 ± 3.3
AC 0.48 ± 0.13 104.9 0.23 ± 0.07 0.40 ± 0.87 2.2 ± 0.9 27.2 ± 15.7 39.0 ± 10.8 36.4 ± 24.8
Tuttlingen NE
Ah1 2.42 ± 0.22 174.8 0.35 ± 0.05 0.33 ± 0.01 6.8 ± 0.9 45.7 ± 5.7 61.0 ± 1.6 61.3 ± 8.1
BA 0.82 ± 0.13 103.8 0.19 ± 0.01 0.37 ± 0.02 4.1 ± 0.7 35.0 ± 2.9 39.9 ± 1.7 24.9 ± 3.4
C1 0.77 ± 0.03 141.9 0.16 ± 0.01 0.35 ± 0.00 4.7 ± 0.2 37.6 ± 1.1 52.5 ± 0.5 47.1 ± 1.6
Schänis
Ah1 1.13 ± 0.21 140.8 0.36 ± 0.13 0.43 ± 0.03 3.3 ± 0.7 44.0 ± 9.8 60.5 ± 2.9 33.0 ± 12.1
Ah2 0.13 ± 0.07 103.0 0.14 ± 0.05 0.46 ± 0.07 0.9 ± 0.4 20.4 ± 11.9 42.8 ± 11.4 38.9 ± 23.5
Bw1 0.09 ± 0.01 77.7 0.05 ± 0.01 0.42 ± 0.03 1.8 ± 0.2 24.3 ± 2.8 33.7 ± 1.7 18.0 ± 4.0
Bärenthal
Ah 1.14 ± 0.15 54.0 0.35 ± 0.02 0.40 ± 0.04 3.2 ± 0.4 25.1 ± 4.3 18.3 ± 1.2 7.5 ± 3.5
BA 0.05 ± 0.03 48.0 0.02 ± 0.00 0.40 ± 0.03 2.3 ± 1.3 19.6 ± 7.2 17.0 ± 3.5 9.0 ± 5.1
Bw 0.003 ± 0.000 92.0 0.01 ± 0.00 0.32 ± 0.03 0.3 ± 0.0 2.7 ± 0.4 8.5 ± 2.5 80.5 ± 2.8