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14 декабря, 2021
2.3.1 Effect of Biomass Ashes on P Uptake and Shoot Biomass
In the field experiments positive results of ash supply were found in Rostock on the loamy sand (Table 2.6), but not in Trenthorst on the sandy loam (Table 2.7). In Rostock in 2007 higher barley yields (significant) and higher P uptakes (by trend) were found after SA and RMA application in comparison with the control. For maize in 2008 the best effects were found again after SA supply but also after CA supply (Table 2.6).
Fertilization |
Summer barley (grain) 2007 |
Maize (whole plant) 2008 |
||
Yield (FM, 14% water) (dtha-1) |
P uptake (kg ha ‘) Yield (DM) (dt ha ‘) Puptake (kg ha ‘) |
|||
0.039* |
0.261 NS |
0.012* |
0.007** |
|
CON |
30.2 a |
11.6 |
162 a |
32.2 a |
SA |
35.3 b |
13.0 |
180 b |
39.2 c |
RMA |
35.5 b |
13.1 |
165 a |
33.3 ab |
CA |
33.6 ab |
12.7 |
179 b |
37.0 bc |
Mean |
33.6 |
12.6 |
172 |
35.4 |
Different characters indicate significant different means at p < 0.05 within a column *p < 0.05; **p < 0.01 FM fresh matter, DM dry matter, CON control, SA straw ash, RMA rape meal ash, CA cereal ash, NS not significant |
Table 2.7 Effect of biomass (sandy loam) |
ashes on yield and |
P uptake, Trenthorst |
field experiment |
|
Fertilization |
Summer wheat (grain) 2007 |
Blue lupin (grain) 2008 |
||
Yield (FM, 14 % water) (dtha-1) |
P uptake (kg ha 1) |
Yield (FM, 14% water) (dt ha-1) |
P uptake (kg ha 1) |
|
0.370 NS |
0.418 NS |
0.184 NS |
0.134 NS |
|
CON |
32.6 |
11.6 |
37.2 |
11.0 |
SA |
31.5 |
11.3 |
37.0 |
10.7 |
RMA |
31.1 |
11.1 |
33.6 |
9.8 |
CA |
31.5 |
11.3 |
36.9 |
10.5 |
Mean |
31.7 |
11.3 |
36.2 |
10.5 |
FM fresh matter, CON control, SA straw ash, RMA rape meal ash, CA cereal ash, NS not significant at p < 0.05 |
The missing effects in the Trenthorst experiment concerning yield and P uptake (Table 2.7) were most probably related to the soil conditions, mainly to the higher pH of this soil (Tables 2.2, 2.10, 2.11). Therefore, the liming effect of biomass ashes did not result in a further adv antage regarding the availability of nutrients, like we expected for sandy soils with lower pH. Furthermore, the soil P content in the Trenthorst soil was higher, which may have masked the P fertilizing effects of the ashes.
Owing to the lower soil volume, the fertilizing effects were higher in the pot experiments than in the field experiments. Significant effects were found for both soils in the 2007 and 2008 experiments.
The crop P uptake increased when P was supplied, independently of whether ash or TSP was added. In 2007, maize showed the highest P uptake of all main crops, with a mean value of 91.3 mg pot-1. In comparison with the control, the maize P uptake rose owing to P supply. The highest increasing rates were found for CA (about 34%) and TSP (about 44%) (Table 2.8). These results are in coherence with the biomass yield of maize (data not shown).
In 2008 on sandy loam, barley, which generated the highest biomass, also had the highest P uptake (especially after RMA supply: 94.6 mg pot-1) (Table 2.9).
Different characters indicate significant different means at p < 0.05 within a column *p < 0.05; **p < 0.01; ***p < 0.001 CON control, TSP triple superphosphate, RMA rape meal ash, SA straw ash, CA cereal ash |
Different characters indicate significant different means atp < 0.05 within a column ***p < 0.001 CON control, TSP triple superphosphate, RMA rape meal ash, SA straw ash, CA cereal ash |
Maize and lupin showed notable positive reactions on CA fertilization, with up to 74% more P uptake than in the control. For the catch crops, the highest P uptakes were found for phacelia and buckwheat in both pot experiments in 2007 and 2008.
Crop-specific P utilizations from the P sources were also relevant. In 2007, usually the highest effects were found for TSP and RMA, whereas the effects of RMA were a little smaller than those of TSP. The opposite was found for lupin and
phacelia, with slightly better results due to RMA. In consequence of the lower P concentration, SA application usually resulted in a lower crop P uptake than the other ashes. For oil radish after SA supply, even lower values were found than in the control without P. However, the P uptake of phacelia in the SA treatment was 36% higher than in the control. The SA effect on the P uptake of phacelia was even comparable to the RMA effect (Table 2.8). Differences in P uptake were also found after CA application, with high values for maize and rather low values for barley and lupin.
These effects underline the crop-specific mechanisms (see also Fig. 2.1) which should be considered when planning ash application within the crop rotation. Plant — specific adaptation mechanisms may warrant a sufficient P supply also under conditions of P deficiency in soil. For example, rape may excrete organic acids in the root zone, which is an effective strategy to increase P uptake mainly on soil with higher pH (Hoffland 1992). Buckwheat has been shown to have different P uptake efficiencies depending on soil conditions (Zhu et al. 2002). According to Van Ray and Van Diest (1979), different plant species differ in their behaviour with respect to uptake of cations. Excessive accumulation of cations within the plant can result in net excretion of H+, and in a lowering of pH values in soil, as was found in our experiments after cultivation of phacelia and buckwheat. Besides such kinds of chemical modifications in the rhizosphere, morphological root adaptations of plants may also help to supply plants with P (Fig. 2.1).
physiological enhanced chemical availability:
• changes in rhizosphere chemistry (pH; redox potential)
•
release of organic acids and enzymes