Table I.
Measurement | Volume | [NH4+] | Atom % 15N | I 14NH4+ | II 15NH4+ | Rate |
---|---|---|---|---|---|---|
L | mm | % | μmol 160 L−1 | μmol plant−1 10 h−1 | ||
A. Initial (9 pm) | 160 | 0.223 | 96.10 | 1392 | 34,288 | |
B. Injection | 0.09756 | 113 | 99.80 | 22 | 11,002 | |
C. Final (7 am) | 160 | 0.231 | 93.55 | 2384 | 34,576 | |
D. Change (C − A − B) | +970 | −10,714 | ||||
E. Mean concentration (A + C)/2 | 1888 | 34,432 | ||||
F. Net 15NH4+ uptake (DII/227 plants) | 47.2 | |||||
G. 14NH4+ uptakea(F[EI/EII]) | 2.6 | |||||
H. Total NH4+ uptake (F + G) | 49.8 | |||||
I. Net 14NH4+ release (DI/227 plants) | 4.3 | |||||
J. “True” 14NH4+ releaseb(I + G) | 6.9 |
Rates of 15NH4+ uptake, 14NH4+ uptake, and 14NH4+ release by 227 maize seedlings were calculated from [15NH4+] and [14NH4+] in the nutrient solution at the beginning (9 pm) and end (7 am) of the first 10-h dark period, during which 97.56 mL of 113 mm 15NH4+ (99.8 atom % 15N) was injected to maintain the total [NH4+] close to its initial level (0.223 mm).
14NH4+ uptake can be estimated from net 15NH4+ uptake because the two isotopic species are taken up in proportion to their mean molar concentrations in the nutrient solution during the uptake period.
Net 14NH4+ release = true 14NH4+ release − 14NH4+ uptake. Therefore, true 14NH4+ release = net 14NH4+ release + 14NH4+ uptake.