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1d947889e4 Oliv*0001 .. include:: ../defs.hrst
                0002 
                0003 .. _Uptake:
                0004 
                0005 Nutrient uptake and limitation
                0006 ^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^
                0007 
a4f2018aab Oliv*0008 The uptake rate of dissolved inorganic carbon is
                0009 
                0010 .. math::
                0011 
                0012    U^{\op{DIC}}_j = P^{\mathrm{C}}_j {c}_j
                0013          - \op{synthcost}\cdot U^{\mathrm{N}}_j
                0014 
                0015 where the carbon specific growth rate, :math:`P^{\op{C}}_j`, is discussed in
                0016 :numref:`Growth`, and the second term is only present with both N and Chl quotas
                0017 and the Geider formulation of photosynthesis.
                0018 
                0019 Nutrient limitation is computed following Liebig's law of the minimum,
                0020 
1d947889e4 Oliv*0021 .. math::
c7b6c66d45 Oliv*0022    :label: eq_darwin_limitnut
1d947889e4 Oliv*0023 
                0024    \gamma^{\op{nut}}_j = \min(\gamma^{\mathrm{P}}_j, \gamma^{\mathrm{N}}_j, \gamma^{\op{Si}}_j,
                0025                               \gamma^{\op{Fe}}_j)
                0026 
a4f2018aab Oliv*0027 We will discuss the limitation terms for each element together with the
                0028 uptake rate of that element for the cases with and without a corresponding
                0029 elemental quota in plankton.
                0030 
1d947889e4 Oliv*0031 Without P quota:
                0032 ''''''''''''''''
                0033 
                0034 Monod limitation
                0035 
                0036 .. math:: \gamma^{\mathrm{P}}_j = \frac{\mathrm{PO}_4}{\mathrm{PO}_4 + k^{\op{PO4}}_j}
                0037 
81872c4188 Oliv*0038 .. math:: U^{\mathrm{P}}_j = R^{{\mathrm{P}}:{\mathrm{C}}}_j U^{\op{DIC}}_j
1d947889e4 Oliv*0039 
                0040 With P quota:
                0041 '''''''''''''
                0042 
                0043 normalized Droop limitation
                0044 
                0045 .. math::
                0046 
                0047    \gamma^{\mathrm{P}}_j = \left[ \frac{1 - Q^{{\mathrm{P}}\min}_j/Q^{{\mathrm{P}}}_j}
                0048                                {1 - Q^{{\mathrm{P}}\min}_j/Q^{{\mathrm{P}}\max}_j}
                0049                    \right]_0^1
                0050 
                0051 .. math::
                0052 
                0053    U^{\mathrm{P}}_j = V^{{\mathrm{P}}\max}_j \frac{\mathrm{PO}_4}{\mathrm{PO}_4 + k^{\op{PO4}}_j}
                0054               {{\text{reg}}}^{Q{\mathrm{P}}}_j \cdot f^{{\text{up}}}_j(T) \cdot {c}_j
                0055 
                0056 where
                0057 
                0058 .. math::
                0059 
                0060      {{\text{reg}}}^{Q{\mathrm{P}}}_j = \left( \left[ \frac{Q^{{\mathrm{P}}\max}_j - Q^{{\mathrm{P}}}_j}
                0061                                 {Q^{{\mathrm{P}}\max}_j - Q^{{\mathrm{P}}\min}_j}
                0062                     \right]_0^1 \right)^{h_{\op{U}}}
                0063 
a4f2018aab Oliv*0064 and the exponent, :math:`h_{\op{U}}`, is the Hill number for uptake (default 1).
1d947889e4 Oliv*0065 
                0066 Si:
                0067 '''
                0068 
                0069 Diatoms (trait :varlink:`hasSi` = 1) have linear limitation when using a Si quota,
                0070 
                0071 .. math::
                0072 
                0073    \gamma^{\op{Si}}_j = \left[ \frac{Q^{\op{Si}}_j - Q^{\op{Si}\min}_j}
                0074                               {Q^{\op{Si}\max}_j - Q^{\op{Si}\min}_j}
                0075                       \right]_0^1
                0076 
                0077 Otherwise Si is analogous to P.
                0078 
                0079 Without N quota:
                0080 ''''''''''''''''
                0081 
                0082 diazotroph:
                0083 """""""""""
                0084 
                0085 No limitation, no consumption:
                0086 
                0087 .. math:: \gamma^{\mathrm{N}}_j = 1
                0088 
                0089 .. math:: U^{\op{NH4}}_j = U^{\op{NO2}}_j = U^{\op{NO3}}_j = 0
                0090 
                0091 not diazotroph:
                0092 """""""""""""""
                0093 
                0094 Modified Monod limitation:
                0095 
                0096 .. math:: \gamma^{\mathrm{N}}_j = \left[ \gamma^{\op{NH4}}_j + \gamma^{\op{NO2}}_j + \gamma^{\op{NO3}}_j \right]_0^1
                0097 
                0098 .. math:: \gamma^{\op{NH4}}_j = \op{useNH4}_j \frac{\op{NH}_4}{\op{NH}_4 + k^{\op{NH4}}_j}
                0099 
                0100 NO\ :sub:`2` and NO\ :sub:`3` limitations can be combined
                0101 (trait :varlink:`combNO` = 1),
                0102 
                0103 .. math::
                0104 
                0105    \gamma^{\op{NO2}}_j = \op{useNO2}_j
                0106      \dfrac{\op{NO}_2}{\op{NO}_2 + \op{NO}_3 + k^{\op{NO3}}_j}
a4f2018aab Oliv*0107      \op{e}^{-\sigma^{\op{amm}}_j \op{NH}_4}
1d947889e4 Oliv*0108 
                0109 .. math::
                0110 
                0111    \gamma^{\op{NO3}}_j = \op{useNO3}_j
                0112      \dfrac{\op{NO}_3}{\op{NO}_2 + \op{NO}_3 + k^{\op{NO3}}_j}
a4f2018aab Oliv*0113      \op{e}^{-\sigma^{\op{amm}}_j \op{NH}_4}
1d947889e4 Oliv*0114 
                0115 or not (combNO = 0),
                0116 
                0117 .. math::
                0118 
                0119    \gamma^{\op{NO2}}_j = \op{useNO2}_j
                0120      \dfrac{\op{NO}_2}{\op{NO}_2 + k^{\op{NO2}}_j}
a4f2018aab Oliv*0121      \op{e}^{-\sigma^{\op{amm}}_j \op{NH}_4}
1d947889e4 Oliv*0122 
                0123 .. math::
                0124 
                0125    \gamma^{\op{NO3}}_j = \op{useNO3}_j
                0126      \dfrac{\op{NO}_3}{\op{NO}_3 + k^{\op{NO3}}_j}
a4f2018aab Oliv*0127      \op{e}^{-\sigma^{\op{amm}}_j \op{NH}_4}
1d947889e4 Oliv*0128 
                0129 Uptake is then
                0130 
                0131 .. math::
                0132    :label: eq_uptakeN
                0133 
                0134      U^{\op{NH4}}_j &= \frac{\gamma^{\op{NH4}}_j}
                0135                     {\gamma^{\op{NH4}}_j + \gamma^{\op{NO2}}_j + \gamma^{\op{NO3}}_j}
81872c4188 Oliv*0136                     R^{{\mathrm{N}}:{\mathrm{C}}}_j U^{\op{DIC}}_j
1d947889e4 Oliv*0137 
                0138      U^{\op{NO2}}_j &= \frac{\gamma^{\op{NO2}}_j}
                0139                     {\gamma^{\op{NH4}}_j + \gamma^{\op{NO2}}_j + \gamma^{\op{NO3}}_j}
81872c4188 Oliv*0140                     R^{{\mathrm{N}}:{\mathrm{C}}}_j U^{\op{DIC}}_j
1d947889e4 Oliv*0141 
                0142      U^{\op{NO3}}_j &= \frac{\gamma^{\op{NO3}}_j}
                0143                      {\gamma^{\op{NH4}}_j + \gamma^{\op{NO2}}_j + \gamma^{\op{NO3}}_j}
81872c4188 Oliv*0144                      R^{{\mathrm{N}}:{\mathrm{C}}}_j U^{\op{DIC}}_j
1d947889e4 Oliv*0145 
                0146 With N quota:
                0147 '''''''''''''
                0148 
                0149 linear limitation
                0150 
                0151 .. math::
                0152 
                0153    \gamma^{\mathrm{N}}_j = \left[ \frac{Q^{{\mathrm{N}}}_j - Q^{{\mathrm{N}}\min}_j}
                0154                            {Q^{{\mathrm{N}}\max}_j - Q^{{\mathrm{N}}\min}_j}
                0155                    \right]_0^1
                0156 
                0157 .. math::
                0158 
                0159      U^{\op{NH4}}_j &= V^{\op{NH4}\max}_j
                0160                     \frac{\op{NH}_4}{\op{NH}_4 + k^{\op{NH4}}_j}
                0161                     {{\text{reg}}}^{Q{\mathrm{N}}}_j \cdot
                0162                     f^{{\text{up}}}_j(T) \cdot {c}_j
                0163 
                0164      U^{\op{NO2}}_j &= V^{\op{NO2}\max}_j \cdot
a4f2018aab Oliv*0165                     {\mathrm{e}}^{-\sigma^{\op{amm}}_j \op{NH}_4} \cdot
1d947889e4 Oliv*0166                     \frac{\op{NO}_2}{\op{NO}_2 + k^{\op{NO2}}_j}
                0167                     {{\text{reg}}}^{Q{\mathrm{N}}}_j \cdot
                0168                     f^{{\text{up}}}_j(T) \cdot {c}_j
                0169 
                0170      U^{\op{NO3}}_j &= V^{\op{NO3}\max}_j \cdot
a4f2018aab Oliv*0171                      {\mathrm{e}}^{-\sigma^{\op{amm}}_j \op{NH}_4} \cdot
1d947889e4 Oliv*0172                      \frac{\op{NO}_3}{\op{NO}_3 + k^{\op{NO3}}_j}
                0173                      {{\text{reg}}}^{Q{\mathrm{N}}}_j \cdot
                0174                      f^{{\text{up}}}_j(T) \cdot {c}_j
a4f2018aab Oliv*0175                      \cdot \gamma^{\op{QFe}}_j
1d947889e4 Oliv*0176 
                0177 where
                0178 
                0179 .. math::
                0180 
                0181    {{\text{reg}}}^{Q{\mathrm{N}}}_j = \left( \left[ \frac{Q^{{\mathrm{N}}\max}_j - Q^{{\mathrm{N}}}_j}
                0182                                 {Q^{{\mathrm{N}}\max}_j - Q^{{\mathrm{N}}\min}_j}
                0183                     \right]_0^1 \right)^{h_{\op{U}}}
                0184 
                0185 diazotroph:
                0186 """""""""""
                0187 
                0188 consume what is available, fix what is missing (up to
                0189 :math:`V^{{\mathrm{N}}\max}_j`),
                0190 
                0191 .. math::
                0192 
                0193    U^{{\mathrm{N}}}_j = \max\biggl( U^{\op{NH4}}_j + U^{\op{NO2}}_j + U^{\op{NO3}}_j,\;
                0194                     V^{{\mathrm{N}}\max}_j
                0195                     {{\text{reg}}}^{Q{\mathrm{N}}}_j \cdot
                0196                     f^{{\text{up}}}_j(T) \cdot {c}_j
                0197                 \biggr) \\
                0198 
                0199 Rate of nitrogen fixation is
                0200 
                0201 .. math:: U^{{\mathrm{N}}}_j - U^{\op{NH4}}_j - U^{\op{NO2}}_j - U^{\op{NO3}}_j
                0202 
                0203 
                0204 not diazotroph:
                0205 """""""""""""""
                0206 
                0207 .. math:: U^{{\mathrm{N}}}_j = U^{\op{NH4}}_j + U^{\op{NO2}}_j + U^{\op{NO3}}_j
                0208 
                0209 
                0210 Without Fe quota:
                0211 '''''''''''''''''
                0212 
                0213 .. math:: \gamma^{\op{Fe}}_j = \frac{\op{FeT}}{\op{FeT}+ k^{\op{Fe}}_j}
                0214 
a4f2018aab Oliv*0215 .. math:: \gamma^{\op{QFe}}_j = 1
1d947889e4 Oliv*0216 
81872c4188 Oliv*0217 .. math:: U^{\op{Fe}}_j = R^{\op{Fe}:{\mathrm{C}}}_j U^{\op{DIC}}_j
1d947889e4 Oliv*0218 
                0219 
                0220 With Fe quota,
                0221 ''''''''''''''
                0222 
                0223 a low iron quota does not directly limit growth,
                0224 
                0225 .. math:: \gamma^{\op{Fe}}_j = 1
                0226 
a4f2018aab Oliv*0227 It rather reduces the light available for photosynthesis (see
                0228 :numref:`Growth` above),
1d947889e4 Oliv*0229 
                0230 .. math::
                0231 
a4f2018aab Oliv*0232    \gamma^{\op{QFe}}_j = \left[ \frac{1 - Q^{\op{Fe}\min}_j/Q^{\op{Fe}}_j}
1d947889e4 Oliv*0233                                    {1 - Q^{\op{Fe}\min}_j/Q^{\op{Fe}\max}_j}
                0234                        \right]_0^1
                0235 
                0236 Iron uptake depends on the available dissolved iron,
                0237 
                0238 .. math::
                0239 
                0240    U^{\op{Fe}}_j = V^{\op{Fe}\max}_j \frac{\op{FeT}}{\op{FeT}+ k^{\op{Fe}}_j}
                0241               {{\text{reg}}}^{Q\op{Fe}}_j \cdot
                0242               f^{{\text{up}}}_j(T) \cdot {c}_j
                0243 
                0244 where
                0245 
                0246 .. math::
                0247 
                0248    {{\text{reg}}}^{Q\op{Fe}}_j = \left( \left[ \frac{Q^{\op{Fe}\max}_j - Q^{\op{Fe}}_j}
                0249                                  {Q^{\op{Fe}\max}_j - Q^{\op{Fe}\min}_j}
                0250                     \right]_0^1 \right)^{h_{\op{U}}}
                0251 
a4f2018aab Oliv*0252 
                0253 Effective half saturation constants
                0254 '''''''''''''''''''''''''''''''''''
                0255 
                0256 If :varlink:`DARWIN_effective_ksat` is true, half saturations for non-quota
                0257 elements are computed from quota traits. If :varlink:`darwin_select_kn_allom`\
                0258 =1 (now deprecated), the half saturation for :math:`\op{NO}_3` is computed
                0259 following Ward et al.,
                0260 
                0261 .. math::
                0262 
                0263    k^{\op{NO3}}_j \rightarrow \frac{ k^{\op{NO3}}_j
                0264                               P^{{\mathrm{C}}{\op{m}}}_j Q^{{\mathrm{N}}\min}_j
                0265                               (Q^{{\mathrm{N}}\max}_j - Q^{{\mathrm{N}}\min}_j) }
                0266                             { V^{\op{NO3}\max}_j Q^{{\mathrm{N}}\max}_j +
                0267                               P^{{\mathrm{C}}{\op{m}}}_j Q^{{\mathrm{N}}\min}_j
                0268                               (Q^{{\mathrm{N}}\max}_j - Q^{{\mathrm{N}}\min}_j) }
                0269 
                0270 and those of the other elements are computed by scaling :math:`k^{\op{NO3}}_j`
                

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0271 with the type’s elemental ratios. Here, :math:`k^{\op{NO3}}_j` on the 0272 right-hand side is computed from :varlink:`a_ksatNO3` and :varlink:`b_ksatNO3`. 0273 0274 If :varlink:`darwin_select_kn_allom`\ =2 (the default), the half saturation for 0275 :math:`\op{NO}_3` is computed following Follett et al., 0276 0277 .. math:: 0278 0279 k^{\op{NO3}}_j \rightarrow k^{\op{NO3}}_j \frac 0280 { P^{{\mathrm{C}}{\op{m}}}_j Q^{{\mathrm{N}}\min}_j } 0281 { V^{\op{NO3}\max}_j } 0282 0283 Those of the other elements are again computed by scaling

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0284 :math:`k^{\op{NO3}}_j` with the type’s elemental ratios. 0285 0286 0287 Uptake and limitation parameters 0288 '''''''''''''''''''''''''''''''' 0289 0290 .. csv-table:: Uptake parameters 0291 :delim: & 0292 :widths: 13,20,17,15,15,20 0293 :class: longtable 0294 :header: Trait, Param, Symbol, Default, Units, Description faa67d1773 Oliv*0295 :name: tab_phys_pkg_darwin_uptake 0296 0297 & :varlink:`synthcost` & :varlink:`synthcost` & 0.0 & mmol C / mmol N & cost of biosynthesis 0298 :varlink:`hasSi` & :varlink:`grp_hasSi` & hasSi\ :math:`_j` & 0 & & 1: uses silica (Diatom), 0: not 0299 :varlink:`diazo` & :varlink:`grp_diazo` & diazo\ :math:`_j` & 0 & & 1: use molecular instead of mineral nitrogen, 0: not 0300 :varlink:`useNH4` & :varlink:`grp_useNH4` & useNH4\ :math:`_j` & 1 & & 1: can use ammonia, 0: not 0301 :varlink:`useNO2` & :varlink:`grp_useNO2` & useNO2\ :math:`_j` & 1 & & 1: can use nitrite, 0: not 0302 :varlink:`useNO3` & :varlink:`grp_useNO3` & useNO3\ :math:`_j` & 1 & & 1: can use nitrate, 0: not 0303 :varlink:`combNO` & :varlink:`grp_combNO` & combNO\ :math:`_j` & 1 & & 1: combined nitrite/nitrate limitation, 0: not 0304 :varlink:`Qnmin` & :varlink:`a <a_Qnmin>`,\ :varlink:`b_Qnmin` & :math:`Q^{\op{N}\min}_j` & 0.07 V\ :sup:`--0.17` & mmol N / mmol C & minimum nitrogen quota 0305 :varlink:`Qnmax` & :varlink:`a <a_Qnmax>`,\ :varlink:`b_Qnmax` & :math:`Q^{\op{N}\op{max}}_j` & 0.25 V\ :sup:`--0.13` & mmol N / mmol C & maximum nitrogen quota 0306 :varlink:`Qpmin` & :varlink:`a <a_Qpmin>`,\ :varlink:`b_Qpmin` & :math:`Q^{\op{P}\min}_j` & 0.002 V\ :sup:`0` & mmol P / mmol C & minimum phosphorus quota 0307 :varlink:`Qpmax` & :varlink:`a <a_Qpmax>`,\ :varlink:`b_Qpmax` & :math:`Q^{\op{P}\op{max}}_j` & 0.01 V\ :sup:`0` & mmol P / mmol C & maximum phosphorus quota 0308 :varlink:`Qsimin` & :varlink:`a <a_Qsimin>`,\ :varlink:`b_Qsimin` & :math:`Q^{\op{Si}\min}_j` & 0.002 V\ :sup:`0` & mmol Si / mmol C & minimum silica quota 0309 :varlink:`Qsimax` & :varlink:`a <a_Qsimax>`,\ :varlink:`b_Qsimax` & :math:`Q^{\op{Si}\op{max}}_j` & 0.004 V\ :sup:`0` & mmol Si / mmol C & maximum silica quota 0310 :varlink:`Qfemin` & :varlink:`a <a_Qfemin>`,\ :varlink:`b_Qfemin` & :math:`Q^{\op{Fe}\min}_j` & 15E-6 V\ :sup:`0` & mmol Fe / mmol C & minimum iron quota 0311 :varlink:`Qfemax` & :varlink:`a <a_Qfemax>`,\ :varlink:`b_Qfemax` & :math:`Q^{\op{Fe}\op{max}}_j` & 80E-6 V\ :sup:`0` & mmol Fe / mmol C & maximum iron quota 0312 :varlink:`vmaxNO3` & :varlink:`a <a_vmaxNO3>`,\ :varlink:`b_vmaxNO3` & :math:`V^{\op{NO3}\op{max}}_j` & (0.26/day) V\ :sup:`--0.27` & mmol N / (mmol C s) & maximum nitrate uptake rate 0313 :varlink:`vmaxNO2` & :varlink:`a <a_vmaxNO2>`,\ :varlink:`b_vmaxNO2` & :math:`V^{\op{NO2}\op{max}}_j` & (0.51/day) V\ :sup:`--0.27` & mmol N / (mmol C s) & maximum nitrite uptake rate 0314 :varlink:`vmaxNH4` & :varlink:`a <a_vmaxNH4>`,\ :varlink:`b_vmaxNH4` & :math:`V^{\op{NH4}\op{max}}_j` & (0.51/day) V\ :sup:`--0.27` & mmol N / (mmol C s) & maximum ammonia uptake rate 0315 :varlink:`vmaxN` & :varlink:`a <a_vmaxN>`,\ :varlink:`b_vmaxN` & :math:`V^{\op{N}\op{max}}_j` & (1.28/day) V\ :sup:`--0.27` & mmol N / (mmol C s) & maximum nitrogen uptake rate for diazotrophs 0316 :varlink:`vmaxPO4` & :varlink:`a <a_vmaxPO4>`,\ :varlink:`b_vmaxPO4` & :math:`V^{\op{PO4}\op{max}}_j` & (0.077/day) V\ :sup:`--0.27` & mmol P / (mmol C s) & maximum phosphate uptake rate 0317 :varlink:`vmaxSiO2` & :varlink:`a <a_vmaxSiO2>`,\ :varlink:`b_vmaxSiO2` & :math:`V^{\op{SiO2}\op{max}}_j` & (0.077/day) V\ :sup:`--0.27` & mmol Si / (mmol C s) & maximum silica uptake rate 0318 :varlink:`vmaxFeT` & :varlink:`a <a_vmaxFeT>`,\ :varlink:`b_vmaxFeT` & :math:`V^{\op{Fe}\op{max}}_j` & (14E-6/day) V\ :sup:`--0.27` & mmol Fe / (mmol C s) & maximum iron uptake rate 0319 :varlink:`ksatNO3` & :varlink:`a <a_ksatNO3>`,\ :varlink:`b_ksatNO3` & :math:`k^{\op{NO3}}_j` & 0.085 V\ :sup:`0.27` & mmol N m\ :sup:`-3` & half-saturation conc. for nitrate uptake/limitation 0320 :varlink:`ksatNO2` & :varlink:`a <a_ksatNO2>`,\ :varlink:`b_ksatNO2` & :math:`k^{\op{NO2}}_j` & 0.17 V\ :sup:`0.27` & mmol N m\ :sup:`-3` & half-saturation conc. for nitrite uptake/limitation 0321 :varlink:`ksatNH4` & :varlink:`a <a_ksatNH4>`,\ :varlink:`b_ksatNH4` & :math:`k^{\op{NH4}}_j` & 0.17 V\ :sup:`0.27` & mmol N m\ :sup:`-3` & half-saturation conc. for ammonia uptake/limitation 0322 :varlink:`ksatPO4` & :varlink:`a <a_ksatPO4>`,\ :varlink:`b_ksatPO4` & :math:`k^{\op{PO4}}_j` & 0.026 V\ :sup:`0.27` & mmol P m\ :sup:`-3` & half-saturation conc. for phosphate uptake/limitation 0323 :varlink:`ksatSiO2` & :varlink:`a <a_ksatSiO2>`,\ :varlink:`b_ksatSiO2` & :math:`k^{\op{SiO2}}_j` & 0.024 V\ :sup:`0.27` & mmol Si m\ :sup:`-3` & half-saturation conc. for silica uptake/limitation 0324 :varlink:`ksatFeT` & :varlink:`a <a_ksatFeT>`,\ :varlink:`b_ksatFeT` & :math:`k^{\op{Fe}}_j` & 80E-6 V\ :sup:`0.27` & mmol Fe m\ :sup:`-3` & half-saturation conc. for iron uptake/limitation 0325 & :varlink:`a_ksatNO2fac` & & 1 & & *used for eff.ksat* 0326 & :varlink:`a_ksatNH4fac` & & 0.5 & & *used for eff.ksat* 0327 :varlink:`R_NC` & :varlink:`a_R_NC` & :math:`R^{\op{N}:\op{C}}_j` & 16/120 & mmol N / mmol C & nitrogen-carbon ratio 0328 :varlink:`R_PC` & :varlink:`a_R_PC` & :math:`R^{\op{P}:\op{C}}_j` & 1/120 & mmol P / mmol C & phosphorus-carbon ratio 0329 :varlink:`R_SiC` & :varlink:`a_R_SiC` & :math:`R^{\op{Si}:\op{C}}_j` & 0 & mmol Si / mmol C & silica-carbon ratio 0330 :varlink:`R_FeC` & :varlink:`a_R_FeC` & :math:`R^{\op{Fe}:\op{C}}_j` & 1E-3/120 & mmol Fe / mmol C & iron-carbon ratio 0331 :varlink:`R_ChlC` & :varlink:`a_R_ChlC` & :math:`R^{\op{chl}c}_j` & 16/120 & mg Chl / mmol C & chlorophyll-carbon ratio 0332 :varlink:`amminhib` & :varlink:`a_amminhib` & :math:`\sigma^{\op{amm}}_j` & 4.6 & m\ :sup:`3` / mmol N & coefficient for NH4 inhibition of NO uptake 0333 & :varlink:`hillnumUptake` & :math:`h^{\op{U}}` & 1.0 & & exponent for limiting quota uptake in nutrient uptake a4f2018aab Oliv*0334