Table 1. Site and stand characteristics of the experiments and total amount of the applied fertilisers. | ||||||||||||
Exp. | Lat. °N | Long. °E | Tempsum d.d. (>5 °C) | Tree species | Started at | Stand age at 2009 | SI a), m | Prod a) , m3 ha–1 a–1 | N, kg ha–1 | P, kg ha–1 | Lime, kg ha–1 | Soil texture b) |
25 | 61.817 | 29.329 | 1239 | Pine | 1958 | 84 | 27.9 | 7.4 | 1676 | 149 | 6000 | SL |
33 | 61.875 | 29.343 | 1234 | Pine | 1958 | 70 | 29.3 | 5.9 | 1908 | 120 | 6000 | LS |
35 | 62.409 | 28.707 | 1168 | Spruce | 1958 | 77 | 18.3 | 8.3 | 714 | 144 | 6000 | SL |
36 | 62.409 | 28.710 | 1168 | Spruce | 1958 | 77 | 19.9 | 8.5 | 714 | 144 | 6000 | SL |
37 | 61.415 | 28.545 | 1240 | Pine | 1958 | 75 | 20.0 | 7.4 | 714 | 109 | 6000 | LS |
38 | 61.416 | 28.542 | 1233 | Pine | 1958 | 75 | 21.5 | 8.2 | 714 | 109 | 6000 | S |
52 | 62.024 | 24.811 | 1154 | Pine | 1959 | 58 | 25.9 | 8.1 | 1496 | 149 | 6000 | LS |
55 | 61.662 | 29.304 | 1170 | Pine | 1959 | 65 | 26.1 | 9.8 | 534 | 69 | 6000 | SL |
56 | 62.927 | 25.607 | 1025 | Pine | 1959 | 76 | 22.8 | 4.5 | 1496 | 149 | 6000 | SL |
57 | 62.935 | 25.678 | 1020 | Spruce | 1959 | 77 | 19.4 | 5.9 | 1496 | 149 | 6000 | SL |
58 | 62.935 | 25.677 | 1024 | Spruce | 1959 | 77 | 21.5 | 6.9 | 1496 | 149 | 6000 | SL |
60 | 62.930 | 25.666 | 1020 | Spruce | 1959 | 77 | 23.0 | 7.7 | 1136 | 109 | 6000 | SL |
64 | 61.493 | 29.066 | 1215 | Pine | 1959 | 90 | 22.0 | 5.3 | 714 | 109 | 6000 | LS |
67 | 61.537 | 29.062 | 1160 | Pine | 1959 | 70 | 21.1 | 9.3 | 714 | 109 | 6000 | SL |
68 | 61.956 | 27.575 | 1147 | Pine | 1959 | 84 | 21.5 | 7.6 | 1404 | 149 | 6000 | S |
73 | 62.759 | 24.747 | 1034 | Pine | 1959 | 55 | 25.9 | 8.0 | 1254 | 160 | 6000 | SL |
75 | 62.913 | 24.571 | 1028 | Pine | 1959 | 54 | 25.3 | 4.9 | 742 | 109 | 6000 | SL |
76 | 62.912 | 24.570 | 1028 | Pine | 1959 | 54 | 26.3 | 5.2 | 742 | 109 | 6000 | SL |
77 | 62.911 | 24.568 | 1028 | Pine | 1959 | 54 | 23.3 | 4.1 | 742 | 109 | 6000 | SL |
82 | 63.300 | 25.340 | 999 | Pine | 1959 | 54 | 17.6 | 3.7 | 965 | 193 | 6000 | SL |
97 | 62.574 | 24.119 | 1074 | Pine | 1960 | 61 | 24.8 | 8.5 | 742 | 193 | 6000 | LS |
98 | 62.579 | 24.125 | 1074 | Pine | 1959 | 60 | 24.5 | 6.9 | 1356 | 69 | 6000 | SL |
103 | 63.215 | 24.624 | 1006 | Pine | 1960 | 58 | 22.2 | 4.2 | 742 | 109 | 6000 | LS |
106 | 63.389 | 24.300 | 1013 | Pine | 1960 | 73 | 15.0 | 3.0 | 1136 | 120 | 6000 | LS |
107 | 63.095 | 24.294 | 1013 | Pine | 1960 | 63 | 18.0 | 2.6 | 742 | 153 | 6000 | LS |
113 | 61.172 | 26.050 | 1251 | Spruce | 1961 | 58 | 28.4 | 12.8 | 1486 | 193 | 6000 | SL |
135 | 67.250 | 23.869 | 791 | Pine | 1961 | 87 | 17.6 | 4.6 | 1194 | 120 | 6000 | SL |
155 | 61.169 | 26.048 | 1250 | Spruce | 1962 | 59 | 28.2 | 13.4 | 1074 | 160 | 6000 | SL |
157 | 61.111 | 26.026 | 1229 | Pine | 1962 | 62 | 24.2 | 7.1 | 1317 | 160 | 5000 | LS |
194 | 66.855 | 27.133 | 754 | Spruce | 1964 | 74 | 19.5 | 1.5 | 1110 | 160 | 6000 | SL |
a) SI is H100 and Prod is the mean annual stem volume production for plots not fertilised with N (4 per experiment). b) Soil texture classes: S = sand, LS = loamy sand and SL = sandy loam. |
Fig. 1. Fertilisation experiments.
Fig. 2. Relative increase in stand production caused by nitrogen fertilisation as a function of mean annual production on unfertilised (no N) plots.
Table 2. Concentrations of elements by fertilisation treatment. Covariates in the ANOVA were effective temperature sum, tree species, i.e. pine (0//1), and mean thickness of the organic layer on plots not fertilised with N. | |||||||||
Variable b) | Treatments a) | ||||||||
Cntrl | N | P | L | NP | NL | PL | NPL | F value c) | |
Organic layer | |||||||||
Ctot, g kg–1 | 442a | 443a | 428ab | 362e | 444a | 403bc | 370de | 396cd | 28.4 |
Ntot, g kg–1 | 12.6b | 15.2a | 12.1b | 10.5c | 15.1a | 14.4a | 10.9c | 14.3a | 60.0 |
C/N | 35.7a | 29.6b | 38.1a | 35.2a | 29.8b | 28.7b | 34.9a | 28.4b | 66.7 |
Catot, mg kg–1 | 2823c | 2960c | 4261c | 8246b | 4378c | 9420ab | 10471a | 10525a | 87.2 |
K tot, mg kg–1 | 769a | 622cd | 734ab | 693bc | 597d | 620d | 738ab | 641cd | 13.6 |
Mgtot, mg kg–1 | 396b | 502b | 386b | 1841a | 491b | 2019a | 2104a | 2231a | 30.5 |
Ptot, mg kg–1 | 796b | 757bc | 946a | 706c | 912a | 714bc | 951a | 966a | 33.4 |
pHCaCl2 | 3.22d | 3.21d | 3.38bc | 4.06a | 3.35cd | 4.07a | 4.19a | 4.18a | 191 |
CaAAA, mg kg–1 | 1964d | 2014d | 2902cd | 5157b | 2963c | 5922ab | 6212a | 6255a | 118 |
KAAA, mg kg–1 | 784a | 581c | 752ab | 687b | 583c | 583c | 704b | 570c | 28.1 |
MgAAA, mg kg–1 | 273b | 347b | 252b | 773a | 337b | 904a | 782a | 912a | 45.3 |
PAAA, mg kg–1 | 230bc | 179de | 270a | 184de | 232bc | 157e | 246ab | 212bcd | 25.9 |
Mineral soil | |||||||||
C, g kg–1 | 25.9bc | 30.5ab | 25.3c | 29.2abc | 29.6abc | 28.4abc | 27.5abc | 31.8a | 4.39 |
Ntot g kg–1 | 1.03cd | 1.25ab | 1.02d | 1.13bcd | 1.20abcd | 1.21abc | 1.05cd | 1.34a | 7.80 |
C/N | 25.9ab | 24.6bc | 25.1abc | 26.1ab | 24.8bc | 23.7c | 27.0a | 24.4bc | 5.51 |
pHCaCl2 | 3.99b | 3.80b | 3.92b | 4.68a | 3.81b | 4.37a | 4.71a | 4.55a | 74.1 |
CaAAA, mg kg–1 | 63c | 78c | 120c | 680a | 105c | 474b | 694a | 683a | 52.2 |
KAAA, mg kg–1 | 31.3a | 30.2a | 32.7a | 33.2a | 29.6a | 27.8a | 32.4a | 30.1a | 2.17 |
MgAAA, mg kg–1 | 11.1b | 15.3b | 12.9b | 83.5a | 16.3b | 80.7a | 81.1a | 86.0a | 42.5 |
PAAA, mg kg–1 | 9.6c | 8.8cd | 12.4a | 7.1de | 11.8ab | 6.1e | 10.0bc | 9.2cd | 20.3 |
a) Cntrl = control, N = nitrogen fertilisation, P = phosphorus fertilisation, L = liming. b) AAA = acid ammonium acetate extraction, tot = dry combustion concentration. c) F value from mixed model ANOVA with covariates. If F7,200 > 3.64, then p < 0.001. |
Table 3. Amounts of elements by fertilisation treatment. Potential covariates in the ANOVA were effective temperature sum, tree species, i.e. pine (0/1), and mean thickness of the organic layer on plots not fertilised with N. | |||||||||
Variable b) | Treatments a) | ||||||||
Cntrl | N | P | L | NP | NL | PL | NPL | F value c) | |
Organic layer | |||||||||
Ctot, Mg ha–1 | 16.8b | 22.8a | 17.5b | 16.0b | 22.5a | 21.0a | 16.4b | 20.5a | 25.2 |
Ntot, kg ha–1 | 488b | 778a | 496b | 468b | 764a | 741a | 485b | 734a | 58.9 |
Catot, kg ha–1 | 112d | 150cd | 177cd | 373b | 221c | 488a | 485a | 545a | 64.9 |
Ptot, kg ha–1 | 30.5e | 38.2cd | 38.8cd | 31.7e | 46.1ab | 36.8d | 42.2bc | 49.8a | 35.6 |
Mineral soil | |||||||||
Ctot, Mg ha–1 | 20.8bc | 24.3ab | 20.3c | 22.6abc | 23.7ab | 22.7abc | 22.6abc | 24.5a | 5.28 |
Ntot, kg ha–1 | 842d | 998a | 822d | 883bcd | 961abc | 977ab | 860c | 1023a | 9.38 |
Org. + min. soil | |||||||||
CaAAA, kg ha–1 | 127d | 162d | 214d | 771bc | 233d | 693c | 862ab | 870a | 88.8 |
PAAA, kg ha–1 | 16.4cd | 16.1cd | 21.2a | 14.0de | 21.5a | 13.2e | 19.4ab | 18.5bc | 33.3 |
a) Cntrl = control, N = nitrogen fertilisation, P = phosphorus fertilisation, L = liming. b) AAA = acid ammonium acetate extraction, tot = dry combustion concentration. c) F value from mixed model ANOVA with covariates. If F7,200 > 3.64, then p < 0.001. |
Table 4. Regression equations for total concentrations of elements as a function of cumulative amounts of fertilisers, and site and tree-stand properties. All coefficients are statistically significant (p < 0.05). | ||||||||
Dependent variables | ||||||||
Organic layer | Mineral soil 0–10 cm | |||||||
Independent variables a) | Ntot g kg–1 | C/N | lnCatot mg kg–1 | Ktot mg kg–1 | Ptot mg kg–1 | ln(Ntot+1) g kg–1 | C/N | |
Constant b) | –4.61 | 50.9 | 7.16 | 237 | 316 | –.278 | 22.3 | |
N, Mg ha–1 | 3.07 | –5.76 | –116 | .0820 | –1.40 | |||
P, kg ha–1 | .000849 | 1.47 | ||||||
Lime, Mg ha–1 | –.208 | .167 | ||||||
Ol. thickn., cm | 1.22 | |||||||
Stand age, a | .0978 | .00701 | 5.77 | 5.56 | ||||
Pine (0/1) | –2.24 | 8.09 | –129 | –.278 | 3.10 | |||
Tempsum, d.d. | .00703 | –.0197 | .000896 | |||||
Fines, % | .0107 | 3.47 | 4.72 | .00680 | ||||
Stones, % | .0531 | |||||||
R2 (obs./pred.) | .667 | .738 | .688 | .441 | .619 | .667 | .256 | |
a) N = cumulative amount of fertilised nitrogen, P = cumulative amount of fertilised phosphorus, Lime = cumulative amount of spread lime, Ol. thickn. = mean organic layer thickness on plots not fertilised with nitrogen, Stand age = stand age at year 2009, Pine = 1, if pine, 0 if spruce, Tempsum = average effective temperature sum, Fines = sum of clay + silt, i.e. under 63 µm fraction, Stones = Volumetric percentage of stones. b) In the logaritmic models the constant has been adjusted to yield the original arithmetic mean by adding a residual variance of the regression model, constant + sf2/2. |
Table 5. Regression equations for pH and concentrations of elements extracted with acid ammonium acetate as a function of cumulative amounts of fertilisers and site and tree-stand properties. All coefficients are statistically significant. | |||||||||||
Dependent variables | |||||||||||
Organic layer | Mineral soil 0–10 cm | ||||||||||
Independent variables a) | pHCaCl2 | CaAAA mg kg–1 | KAAA mg kg–1 | PAAA mg kg–1 | pHCaCl2 | lnCaAAA mg kg–1 | lnKAAA mg kg–1 | lnPAAA mg kg–1 | |||
Constant b) | 3.88 | 2879 | 932 | 163 | 3.31 | 4.00 | 2.29 | 1.97 | |||
N, Mg ha–1 | –.0874 | –135 | –33.7 | –.248 | –.207 | ||||||
P, kg ha–1 | .412 | .00295 | |||||||||
Lime, Mg ha–1 | .139 | .562 | –6.46 | –4.75 | .114 | .360 | –.0464 | ||||
Ol. thickn., cm | –.120 | –.240 | –.163 | –.150 | |||||||
Stand age, a | 5.27 | ||||||||||
Pine (0/1) | –.342 | –1222 | .421 | ||||||||
Tempsum, d.d. | –.495 | .000855 | |||||||||
Fines, % | 1.96 | .0101 | .0292 | .0189 | .0231 | ||||||
Stones, % | .00565 | ||||||||||
R2 (obs./pred.) | .811 | .756 | .442 | .346 | .646 | .575 | .583 | .540 | |||
a) N = cumulative amount of fertilised nitrogen, P = cumulative amount of fertilised phosphorus, Lime = cumulative amount of spread lime, Ol. thickn. = mean organic layer thickness on plots not fertilised with nitrogen, Stand age = stand age at year 2009, Pine = 1, if pine, 0 if spruce, Tempsum = average effective temperature sum, Fines = sum of clay + silt, i.e. under 63 µm fraction, Stones = Volumetric percentage of stones. b) In the logaritmic models the constant has been adjusted to yield the original arithmetic mean by adding a residual variance of the regression model, constant + sf2/2. |
Table 6. Regression equations for total amounts of elements as a function of cumulative amounts of fertilisers, and site and tree-stand properties. All coefficients are statistically significant. | |||||||
Dependent variables | |||||||
Organic layer | Mineral soil 0–10 cm | ||||||
Independent variables a) | Ctot kg ha–1 | Ntot kg ha–1 | lnCatot kg ha–1 | Ktot kg ha–1 | Ptot kg ha–1 | lnCtot, kg ha–1 | lnNtot, kg ha–1 |
Constant b) | 8898 | 579 | 5.01 | 35.7 | 39.7 | 8.21 | 5.28 |
N, Mg ha–1 | 4476 | 245 | .139 | 6.31 | .104 | .158 | |
P, kg ha–1 | .000829 | .0727 | |||||
Lime, Mg ha–1 | –229 | –4.10 | .181 | .325 | .00769 | ||
Tempsum, d.d. | .00148 | .00134 | |||||
Ol. thickn., cm | 2562 | ||||||
Fines, % | .00957 | .00845 | |||||
Pine (0/1) | –125 | –.338 | –8.01 | –.278 | –.405 | ||
R2 (obs./pred.) | .400 | .544 | .593 | .192 | .468 | .578 | .641 |
a) N = cumulative amount of fertilised nitrogen, P = cumulative amount of fertilised phosphorus, Lime = cumulative amount of spread lime, Ol. thickn. = mean organic layer thickness on plots not fertilised with nitrogen, Pine = 1, if pine, 0 if spruce, Tempsum = average effective temperature sum, Fines = sum of clay + silt, i.e. under 63 µm fraction. b) In the logaritmic models the constant has been adjusted to yield the original arithmetic mean by adding a residual variance of the regression model, constant + sf2/2. |
Table 7. Regression equations for elemental amounts extracted with acid ammoníum acetate as a function of cumulative amounts of fertilisers and site and tree-stand properties. All coefficients are statistically significant. | ||||||||||
Dependent variables | ||||||||||
Organic layer | Mineral soil 0–10 cm | |||||||||
Independent variables a) | CaAAA kg ha–1 | KAAA kg ha–1 | PAAA kg ha–1 | SAAA kg ha–1 | lnCaAAA kg ha–1 | lnKAAA kg ha–1 | lnPAAA kg ha–1 | SAAA kg ha–1 | ||
Constant b) | 121 | 23.9 | –5.65 | –2.34 | 5.78 | 2.43 | 1.649 | 2.823 | ||
N, Mg ha–1 | 19.2 | 1.14 | .756 | –.206 | .0854 | .201 | ||||
P, kg ha–1 | .0193 | .00283 | .00302 | |||||||
Lime, Mg ha–1 | 29.4 | –.113 | .36 | –.0477 | –.0983 | |||||
Tempsum, d.d. | .000781 | |||||||||
Ol. thickn., cm | 3.78 | 2.29 | .786 | –.305 | –.118 | |||||
Fines, % | .0246 | .012 | .0165 | |||||||
Stones, % | –.0065 | –.00832 | ||||||||
Pine (0/1) | –59.8 | –8.28 | –2.86 | |||||||
Stand age, a | .123 | .065 | –.024 | .0114 | ||||||
R2 (obs./pred.) | .67 | .235 | .469 | .348 | .624 | .505 | .433 | .380 | ||
a) N = cumulative amount of fertilised nitrogen, P = cumulative amount of fertilised phosphorus, Lime = cumulative amount of spread lime, Ol. thickn. = mean organic layer thickness on plots not fertilised with nitrogen, Stand age = stand age at year 2009, Pine = 1, if pine, 0 if spruce, Tempsum = average effective temperature sum, Fines = sum of clay + silt, i.e. under 63 µm fraction, Stones = Volumetric percentage of stones. b) In the logaritmic models the constant has been adjusted to yield the original arithmetic mean by adding a residual variance of the regression model, constant + sf2/2. |
Fig. 3. Relative surplus of N in the organic layer, i.e. (amount of N on the fertilised plots – amount of N on the non-fertilised plots)/amount of N in fertilisers, as a function of the C/N ratio in the organic layer on the unfertilized plots.