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[SSSP home]
| Model |
Photobacterium
phosphoreum: Microbial spoilage model for fresh
MAP fish |
| Reference |
Dalgaard, P., Mejlholm, O. and
Huss, H.H.
(1997a). Application of an iterative approach for development of a microbial model
predicting the shelf-life of packed fish. Int. J. Food Microbiol. 38,
169-179 |
| Primary growth model |
Log-transformed 3-parameter Logistic
model |
| Secondary growth model |
Polynomial model (quadratic)
and square-root model |
| Factor(s) in model |
Temperature and
%CO2 |
| Product validation studies |
- MAP cod fillets, MAP plaice fillets, MAP salmon steaks (Dalgaard
et al. 1997a; Dalgaard 1999, unpublished data from DTU Aqua)
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| Range of applicability |
- MAP cod fillets at
0-15°C with 0–100 % CO2
- MAP plaice fillets at 0-15°C with 0–100 % CO2
- MAP salmon steaks at 0-15°C with 0–100 % CO2
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| Photobacterium phosphoreum is the specific spoilage organism
(SSO)
that limits shelf-life of fresh marine fish when stored in modified atmosphere
packaging (MAP). P.
photobacterium grows without a lag phase and the log-transformed 3-parameter Logistic
model (Eqn. 1) is appropriate as a primary growth model. |
| In eqn. 1, Nt (cfu/g) is the concentration of P. phosphoreum at time t,
N0
(cfu/g) the initial concentration of P. phosphoreum, Nmax the maximum
concentration (cfu/g) and mmax
the maximum specific growth rate (h -1). |
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Figure 1. Log-transformed Logistic model fitted to data for growth of P. phosphoreum in naturally contaminated
cod fillets stored at 0oC in an atmosphere with 100% N2. As
indicated by the arrows, sensory spoilage was observed some time after P. phosphoreum
reached its maximum cell concentration (Dalgaard et al. 1997a) |
| The end of shelf-life for MAP cod fillets has been observed four generation
times (tgen = Ln(2)/µmax) after the inflection point (ti) on the Logistic growth model
(See Figure above).
Consequently, a particular minimal spoilage level was not identified. However, the inflection point is the time when Nt is equal to Nmax/2
and shelf- life can be calculated by the shelf-life criterion shown
below (Eqn. 2): |
|
Eqn.
2
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Shelf-life is calculated from the initial concentration of P. phosphoreum and from
its maximum specific growth rate (mmax). The initial
numbers of P. phosphoreum can be determined in fresh fish by a specific conductance
based method (Dalgaard et al., 1996).
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Secondary growth models:
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Eqn. 3
Eqn. 4
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| Figure 2. Observed and predicted growth of
Photobacterium phosphoreum in fresh MAP cod fillets (Dalgaard et
al. 1997) |
| The effect of temperature and CO2 on
the maximum specific growth rate (mmax) of P.
phosphoreum in MAP cod fillets can be predicted by a quadratic polynomial model
(Eqn. 3). A square-root model (Eqn. 4) is used for MAP plaice and MAP salmon. These
secondary models allow growth of P. phosphoreum to be predicted in fresh
fish stored in modified atmospheres with CO2/N2 gas mixtures.
See e.g. the Figure above for growth of P. phosphoreum in fresh MAP cod fillets. In fact, observed and predicted mmax-values from 11 storage trials
with MAP cod resulted in bias- and accuracy factor values of 0.98 and 1.19, respectively,
and this shows that the model predicted growth rates accurately (Dalgaard, 1999). In addition,
in product storage
trials the model only underestimated shelf-life by 9% on average (See Table just
below). |
Observed and predicted shelf-life of MAP cod fillets stored at constant and at varying
temperatures
| Initial storage temp. |
0oC |
0oC |
0oC |
5oC |
| Final storage temp. |
0oC |
5oC |
10oC |
0oC |
| Winter experiments |
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| Observed shelf-life, days |
15.8 |
8.2 |
6.4 |
9.3 |
| Predicted shelf-life, days |
13.9 (-12 %)a |
8.1 (- 2 %) |
6..1 (- 4 %) |
8.5 (- 9 %) |
| Summer experiments |
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| Observed shelf-life, days |
16.8 |
9.2 |
5.9 |
11.8 |
| Predicted shelf-life, days |
14.7 (-13 %) |
8.0 (-13 %) |
5.4 (- 8 %) |
10.3 (-13 %) |
a % deviation between observed and predicted shelf-life
Effect of MAP on Photobacterium phosphoreum
It is important to use the equilibrium
concentration of CO2 when predicting the effect of MAP on the maximum
specific growth
rate (mmax) of microorganisms. As an example cod fillets packed with
an initial CO2 concentration of 60% and a gas/fish ratio of 2:1
(i.e. 200 ml gas and 100 g of fish) will have an equilibrium concentration of
close to 40% CO2 because CO2 is dissolved in the fish flesh.
With the same initial CO2 concentration but a gas/fish ratio of 4:1
(i.e. 400 ml gas and 100 g of fish) the equilibrium concentration of CO2
will be
close to 50% CO2. To allow users of SSSP to conveniently calculate
equilibrium concentrations of CO2 in fresh MAP fish a specific
module has been included in the software (See the SSSP dialog box below). SSSP calculates equilibrium concentrations of CO2
as a function of storage temperature, initial gas/product ratio and initial
concentration of CO2 in the headspace gas (Ross and Dalgaard 2004 page 129-131).
Follow this link for further details on equations used
to calculation equilibrium concentrations of CO2.
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Effect of gas mixtures with high conncentrations of both CO2
and O2
Oxygen reduces the growth rate of Photobacterium phosphoreum
compared to atmospheres without oxygen (Dalgaard,
1993, Guldager et al. 1998). Furthermore, it has been shown that growth of Photobacterium phosphoreum
can be markedly reduced by packaging of seafood in atmospheres with high
concentration of both CO2 and 02. This has been
observed e.g. for farmed MAP cod, farmed MAP halibut, and MAP tuna (Emborg
et al. 2005, Hansen et al. 2007, Hovda et al. 2007, Sivertsvik, 2007).
However, this marked effect has not been observed in all studies with high
concentration of both CO2 and O2 (Dalgaard et
al. 1997b). For captured/wild fresh MAP cod fillets,
shelf-life at 2°C was extended by 1-2 days when 20% of the nitrogen in MAP was
replaced by 20% pure oxygen (Guldager et al., 1998). The effect of atmospheres
with high concentration of both CO2 and O2 has
not yet been included in the SSSP software. Consequently, SSSP may underestimate the shelf-life of
fresh MAP fish stored in gas mixtures containing high concentrations of oxygen together with
high concentrations of CO2. |
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