|
|
|||
Warning, /doc/phys_pkgs/darwin_uptake.rst is written in an unsupported language. File is not indexed.
view on githubraw file Latest commit c7b6c66d on 2022-03-19 18:19:30 UTC1d947889e4 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`** Warning **
Wide character in print at /usr/local/share/lxr/source line 1030, <$git> line 272.
0271 with the type’s elemental ratios. Here, :math:`k^{\op{NO3}}_j` on the 0272 right-hand side is computed from :varlink:`a_ksatNO3` and :varlink:`b_ksatNO3`. 0273 0274 If :varlink:`darwin_select_kn_allom`\ =2 (the default), the half saturation for 0275 :math:`\op{NO}_3` is computed following Follett et al., 0276 0277 .. math:: 0278 0279 k^{\op{NO3}}_j \rightarrow k^{\op{NO3}}_j \frac 0280 { P^{{\mathrm{C}}{\op{m}}}_j Q^{{\mathrm{N}}\min}_j } 0281 { V^{\op{NO3}\max}_j } 0282 0283 Those of the other elements are again computed by scaling** Warning **
Wide character in print at /usr/local/share/lxr/source line 1030, <$git> line 285.
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
| [ Source navigation ] | [ Diff markup ] | [ Identifier search ] | [ general search ] |
|
This page was automatically generated from https://github.com/darwinproject/darwin3 by the 2.3.7-MITgcm-0.1 LXR engine. The LXR team |
|