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drivers of soil respiration of root and microbial ... - Unitus DSpace

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The distribution <strong>of</strong> N between shoots <strong>and</strong> <strong>root</strong>s also varied depending on the growth stage:<br />

under NH4 + -N 72% <strong>of</strong> the 15 N was recovered in shoots <strong>of</strong> V6 corn, on V8 stage only 58% <strong>of</strong> the<br />

found 15 N had a shoot origin. Under NO3 - -N the difference between two growing stages in<br />

distribution <strong>of</strong> absorbed 15 N was not so clear: 67% <strong>and</strong> 62% <strong>of</strong> recovered 15 N respectively for V6<br />

<strong>and</strong> V8 plants had a shoot origin (Fig. 5).<br />

15 N recovered in BG <strong>and</strong> AG biomass (mmol g dw -1 )<br />

0.6<br />

0.5<br />

0.4<br />

0.3<br />

0.2<br />

0.1<br />

0.0<br />

0.1<br />

0.2<br />

0.3<br />

e<br />

(41%)<br />

(59%)<br />

a<br />

lupine<br />

f<br />

(36%)<br />

(64%)<br />

a<br />

NH 4 + NO 3 -<br />

corn V6 corn V8<br />

a<br />

(72%)<br />

(28%)<br />

a<br />

b<br />

(67%)<br />

(33%)<br />

b<br />

+ -<br />

NH NO<br />

4<br />

3<br />

c<br />

(58%)<br />

(42%)<br />

a<br />

NH 4 +<br />

d<br />

(62%)<br />

Fig. 5. 15 N amount recovered from shoot (above zero) <strong>and</strong> <strong>root</strong>s (below zero. In red) <strong>of</strong> Lupinus albus <strong>and</strong> Zea<br />

mays on V6 <strong>and</strong> V8 growing stage. Percentages indicate 15 N distribution between shoots <strong>and</strong> <strong>root</strong>s <strong>of</strong> plants.<br />

Letters indicate the significance <strong>of</strong> the differences at p=0.05 between the treatments.<br />

5.3.4. Total CO2 efflux from planted <strong>soil</strong> with Lupinus albus <strong>and</strong> Zea mays (V6)<br />

The difference between total CO 2 efflux from the <strong>root</strong>-<strong>soil</strong> system <strong>and</strong> <strong>microbial</strong> <strong>respiration</strong><br />

from bare <strong>soil</strong> incubated at the same conditions was used to calculate the CO2 respired by <strong>root</strong>s <strong>and</strong><br />

associated rhizosphere microorganisms (<strong>root</strong>-derived <strong>respiration</strong>) <strong>and</strong> to compare with the results<br />

from 14 C labeling for <strong>root</strong>-derived CO 2 .<br />

(38%)<br />

b<br />

- NO3 133

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