Diffusion, Boundarv Lavers and the Uptake of Nutrients bv Aquatic Macrophvtes Jeffrey JuIius MacFarlane B.Sc. (Hons. ) Botany Department The University of Adelaiile. Submitted for the Degree of Doctor of Philosophy, June, 1985. tlsl¡tt flnrocbd To my Father : Friend and Master Teacher CONTENTS Summary vrt Dec Iaration tx Acknowl edgement s x INTRODUCTION 1 I.The Kinetics of Heterogeneous Reactions 2 (i) Nernst's TheorY 2 ii ) Modifications of Nernst's Theory ( 6 (iii) Physical basis for kt 9 (iv) FIuid mechanical description of kT 13 (v) Conclusions 20 II.Diffusion and Simultaneous Chemical Reaction 2I (i) Equations for diffusion-reaction 2L ii ) Determination of the extent of ( internal diffusion limitations 25 III. Diffusion Boundary Layers and Nutrient Uptake in Aquatic PIants 2'7 (i) Previous studies 2B (ii) This work 35 MATERIALS AND METHODS 37 ( i ) PIants 37 ( ii ) solutions 3B ( iii ) ResPiration 40 ( iv ) Photosynthesis 42 (v) Uptake of methylamine and phosphate 4B (vi) Stirring gradient tower 49 (iíi) MEMBRANE TRANSPORT 53 r . uptake of I l ac ] uethylamine by UIva qrgrqa 53 ( i ) Results 53 (ii) Boundary layer Iimitations and V 54 (iii) The effect of stirring at high methylamine concentrations 54 (iv) The saturation of influx with stirring 56 (v) Comparison of observed with predicted kinet¡cs 57 (vi) other ctnolyses 60 rr.uptake of l32plehosphate by ulva rrglda 62 r4c]uetrrylamine rrr.uptake of 1,32p lPhosphate and I by Vallisneria spiralis 7I i ) Results 7l ( ( ii ) Discussion 72 RESPIRATION I.Kinetics of OxYgen Reduction 75 II Respiration in Ulva rl-grqq . BO ( i ) Results 80 ( ii ) Discussion BI III. Respiration of Vallisneria sPiralis 89 PHOTOSYNTHESIS 94 I.Photosynthesis of Ulva rfg-Lqq 94 ( i ) Results 94 ii ) A note on the meaning of ( KM for photosynthetic CO2 fixation 99 (iii) Photosynthesis at low 100 PH (iv) Oxygen inhibition of photosynthesis 104 (iv¡ (v) Photosynthesis at higher PH's 107 (vi) Mechanisms of HCOã use II4 Il.Photosynthesis of Amphibol is antarctica and Vallisneria spiralis r20 ( i ) Results t20 ( ii ) C supply for photosynthesis of A. antarctica r23 ( iii ) C supply for photosynthesis of V. spiralis r26 CONCLUSIONS 133 Appendix I Fick's Laws I4I Appendix II : Origin of the Quadratic Describing an Enzyme-Catalysed Reaction in Series with a Diffusion Resistance 143 Appendix III : The Meaning of the APParent Kt for an Enzyme-Catalysed Reaction in Series with a TransPort Proce s s 145 Appendix IV : Relaxation of Diffusion to a FIat Plate I47 Appendix V Diffusion and Reaction in ParaI I e I r50 (i) The diffusion-reaction equation ts0 (ii) First-order kinetics I52 ( iii ) Zeroth-order kinetics I57 (v) SUMMARY Diffusion limitations on the influxes of tI4C] methylamine and l32pl phosphate, and oî the respi ratory uptake of o2r have been examined in the marine macroalga Ulva rlgida and the freshwater angiospe rm Vallisneria spiralis; photosynthetic 02 evolution (and fixation of l4c-1abe11ed inorganic carbon) has also been studied in these two plants and in the marine angiosperm phibol is Am antarctica. In Ulva, the influx of methylamine and the apparent "KM" of the process are greatly affected by the rate of stirring of the bulk medium. The kinetics of the influx are directly predicted by an equation of the Michaelis-Menten form which includes a term for the rate of transport of methylamine through the boundary layer (the Briggs-MaskeIl equation). Transport coefficients range f rom ,.U =-I in a barely-moving solution to ft" nearly 40 ¡rm s-1 in a well stirred one, with a / corresponding change in Ku f rom 20 to tO The Æ. equation is also directly applicable to the photosynthesis of the alga at low pH provided that O2 inhibition can be neglected. The equation is not directly appticable to H2PO4 influx, respiratory O2 uptake or photosynthetic CO2 fixation at high pH. H2PO 4 ')_ influx is complicated by the concomitant flux of HPoî which effectively increases the concentration of H2PO 4 at the plasmalemma. 02 uptake in dark respiration has a complex relationship with the bulk concentration of o2, (vii) and the kinetics are not necessarily first-order Michaelis-Menten; consequently the Briggs-MaskelI equation is invalid. Rates of photosynthesis that are observed at high pH could notbe attained if CO2 was the only inorganic carbon species transporting carbon through the unstirred Iayer. The alga probably uses HCOJ ions directly from the bulk solution as a carbon source and so again the Briggs-Maskell equation, in terms of CO2 fixation, does not hold. The photosynthesis of A[phibolis has a similar response to CO2 and pH as that of UIva - again the Briggs-MaskeIl equation is not directly applicable. Vallisneria leaves have a cuticle which has such a high resistance to the movement of solutes that boundary Iayer Iimitations are negligible. The Ieaves also have a substantial supply of endogenous COZ. Here the cuticle is a distinct advantage because it increases the probabitity of a COZ molecule being assimilated rather than escaping into the bulk medium; this source of CO2 (originally derived from the sediment? ) is probably much more important than the COZ in the surrounding water. (vii i ) ACKNOWLEDGEMENTS This work was carried out under the supervision of Dr. F.A. Smith, who was the ever-encouraging driving force for this rather unsteady flux. I should also I ike to thank others in the Botany Department - Drs. J.T. Wiskich and G.G. Ganf for many varied and stimulating discussions, Prof - H-8.S. Womersley, Dr R. sinclair and B.c. Rowland for advice, Dr. E. Robertson for culture room space, Ian Dry and Patrick Hone for some good talks, and Jane Gibson and Anthony Fox for company. Outwith the Botany Department, I acknowledge the help given by B.C. van Wageningen in translating some German scientific papers, the computer time allowed by Prof. N.A. Wa1ker and the patience of Prof. J.A. Raven. FinaIIy, to my wife, Carol, for typing the manuscript, for numerous calculations, fot support and for a sma1I portion of her indomitable spirit. (x)
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