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. 1998 Nov;118(3):835–841. doi: 10.1104/pp.118.3.835

Table I.

Calculation of NH4+ fluxes into and out of maize roots

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).

a

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. 

b

Net 14NH4+ release = true 14NH4+ release − 14NH4+ uptake. Therefore, true 14NH4+ release = net 14NH4+ release + 14NH4+ uptake.