641
1 INTRODUCTION
Coffea Arabica and Coffea Canephora var. Robusta
there are two main species of coffee. About 60% of the
world’s coffee production is Arabica and 40% is
Robusta. The largest Arabica coffee producers are
situated in Brazil, Colombia and Ethiopia. In turn, the
largest producers of Robusta are Viet Nam, Uganda
and India [11]. According to Goneli et al. [6], in the
world there are two main methods of processing
coffee beans: dry method and wet method. The
applied process significantly influences the selection
of appropriate the coffee beans storage and transport
conditions.
According to the data presented by the
International Coffee Organisation (ICO), global coffee
production has increased by more than 60% since the
1990s. The value of annual coffee exports during last
30 years has increased more than four times from 8.4
billion USD in 1991 to 35.6 billion USD in 2018. he
global coffee trade is characterized by two main
markets: the commodity market, which mainly offers
standard-quality bulk coffee produced in high
volumes and the specialty market, which offers higher
prices for coffee exporters handling lower volumes of
higher-quality coffee beans [11].
Coffee is one of the most popular beverages
consumed in the whole world. According to data
presented in the Coffee Development Report [11],
Europe’s coffee consumption in years 2019/20 was
estimated 55.09 million bags and has grown by an
average annual rate of about 1.3% from 38.41 million
Hygroscopic Properties of Green Coffee Transported
by
Sea
M
. Ruszkowska
1
, P. Dmowski
1
& K. Urbanowicz
2
1
Gdynia Maritime University, Gdynia, Poland
2
Mega Coffee, Kwidzyn, Poland
ABSTRACT: The aim of research was to evaluate the hygroscopic properties of green coffee beans determining
its quality during sea transportation. The research material consisted of seven samples of unroasted bean coffee
from different countries of origin (Kenya, India, Ethiopia, Columbia and Guatemala) obtained directly from the
coffee producer. The water content of green coffee must not exceed 12% as it then has a tendency to grow
mou
ld and become musty. Coffee beans require particular temperature, humidity/moisture and possibly
ventilation conditions and therefore, to explore and predict the behaviour during transport of green coffee its
equilibrium moisture content must be determined for a range of transport temperatures and relative humidity
levels . The present paper focuses on the evaluation of the hygroscopic properties of green coffee from different
countries of origin based on isotherms of water vapour sorption and characteristic selected parameters of the
surface microstructure determining transport conditions and the microbiological stability of this cargo. While
assessing the quality and transport durability of green coffee beans, based on the parameters of monomolecular
layer capacity and the specific surface area of sorption, it was found that especially samples of coffee from
Guatemala and Ethiopia were the least susceptible to changes in the transport conditions.
http://www.transnav.eu
the International Journal
on Marine
Navigation
and Safety of Sea Transportation
Volume 15
Number 3
September 2021
DOI: 10.12716/1001.15.03.19
642
bags in year 1990/91. The European Union (EU) is by
far the largest coffee consumer globally and accounts
for 82% of regional demand within the continent. In
2019/20, coffee consumption in the EU amounted to
45.05 million bags. Among the EU members,
Germany, France, and Italy are the three largest
consumer countries, accounting for 45% of total
consumption in whole Europe. Around 70% of the
European Union coffee imports include unprocessed
coffee imported mainly from Brazil, Viet Nam and
Honduras. More than 90% of coffee is still shipped in
green form. However, it must be stressed that, since
the beginning of 2020, the Covid-19 pandemic has
exacerbated the situation of producing countries
affected by low prices and volatility. The global
spread of the virus, in addition to its dramatic effect
on public health, has resulted in supply chain
disruptions and influenced global demand for coffee.
Coffee is transported from producer to consumer
nations in bulk or in sacks, mostly in containers
holding to 22 tonnes. During the transport even well-
dried coffee contains a great deal of water (about 12%)
that, as long as it remains evenly distributed, do not
poses the problem. However, temperature
fluctuations, that may occured during sea transport,
can cause condensation of water. And as a
consequence of re-wetting fungal and moulds may
growth [7]. Because coffee beans are sensitive to
moisture they are usually shipped in jute or sisal bags
which allows free circulation of air [2]. The net weight
of bags depend on the country of origin of coffee
beans. Coffee bags from Africa are generally 60 kg but
bags from Central America, especially from Colombia
may weigh 69 kg. Over 90% of the European coffee
imports are already transported in ventilated
containers. In sea transport, it is very important to
assign the cargo to a particular class of storage climate
conditions (SCC group). It is carried out based on the
requirements that cargo during the transport process.
In sea transport coffee like tea requires particular
temperature, humidity and ventilation conditions.
Green coffee belongs to the group of loads with the
third biotic activity, for which respiration is
essentially suspended, but biochemical and
microbiological processes are continue. Green coffee
belongs to the group of loads with the third biotic
activity, for which respiration is essentially
suspended, but biochemical and microbiological
processes are continue. Inadequate ventilation may
result in fermentation and rotting of the coffee beans.
It is the result of increased CO
2 levels and to low
supply of atmospheric oxygen [33].
Taking into consideration the required transport
conditions, coffee is classified in the SC VI group of
cargo. This group includes cargoes with a low and
medium water content from 1.5% to 30% in dry mass.
[28]. In general, temperatures during transport of
green coffee beans should range between 10 and 20°C,
because there is a connection between fluctuations in
the ambient temperature and the formation of
condensation water in the container. During the
transport from a hot climate (e.g. Brasil) to a cold
climate (e.g. Poland) the high temperature gradients
are possible and therefor. It is very important that the
temperature inside of container with coffee should not
drop below zero Celsius degrees, because a sudden
drop in temperature leads to higher probability of
condensation water formation in the container and
directly on the cargo and thus causes considerable
cargo losses. Therefor the preventing the formation of
condensation water in the hold is essential and
constitutes the number one priority during sea
transportation. Hence, the cargo in the container
should be protected from dripping water by the use of
appropriate mats. To ensure adequate ventilation, a
sufficient distance the spacing from the cargo is also
necessary. As per the sorption isotherm for green
coffee beans, with 8.5 10% water content are at
equilibrium with relative humidity of 50 65%. If
coffee beans have an excessively high moisture
content, there is a risk of mustiness, mould growth
and post or overfermentation [9, 34].
According to Baptestini et al. [1] temperature and
relative humidity of the environment surrounding the
product are the primary parameters to be considered
during transport. Due to its low moisture content,
roasted and ground coffee may absorb moisture from
the environment, causing clumping and and thus
increasing economic losses. The key metric for
assessing water sorption during transport and storage
are the sorption isotherms.
Taking into account all the above facts, it is
necessary to know the relationship between the air
temperature and relative humidity, and desirable
conditions for transport the product. To obtain this
information, sorption isotherms are indispensable,
which are efficient tools to determine thermodynamic
interactions between the water and food components.
[6].
Given these reasons the objective of this study was
to determine the adsorption isotherms of green bean
coffee. Additionally, this study sought to determine
the thermodynamic properties of water sorption as a
function of water activity (a
w).
2 RESEARCH MATERIAL AND METHODS
The research material included seven green coffee
bean samples imported to Poland by sea from India
(samples I, II and V), Ethiopia (samples III and IV)
and one sample from Columbia (VI) and Guatemala
(VII). The samples of green coffee bean were
processed in two different ways: dry method
(Ethiopia IV and India V) or natural form and wet
method (India I, II, Ethiopia III, Columbia VI and
Guatemala VII).
The tested green coffee bean samples were
subjected to a preliminary analysis by the
determination of the initial water content. Each
samples moisture content was determined by oven-
drying method as recommended for ISO standard ISO
66732005: Green coffee Determination of loss in
mass at 105 degrees Celsius. For water activity (a
w)
measurement, AquaLab 4TE apparatus with an
accuracy of ± 0.003 at 20°C was used (AS4 2,14.0 2017,
Decagon Device Inc., Pullman, WA, USA).
Isotherms of adsorption were determined by the
static method, based on moisture equilibrium between
the tested product samples and the atmosphere of
defined relative humidity, adjusted by means of salt
643
solutions [5]. The determination of adsorption
isotherms was carried out at 20°C±1°C in a range of
water activity a
w=0.07÷0.98. Time fixture equilibrium
was 30 days. Based on the initial weight of the
product and the growth or loss of water content
equilibrium water content was calculated and
sorption isotherms were plotted.
For the purpose for mathematical description of
empirically determined sorption isotherms and
performance of sorption feature characterisation of
the tested green coffee bean samples, sorption
isotherms rearrangements were made by using the
BET equation (1). The water activity (aw) ranged
from 0.07 to 0.98 [22].
( )
( )
111
mw
ww
V Ca
V
a Ca
=

+−

(1)
where:
a
wwater activity [-],
Vadsorption [g H
2O/100g d.m.],
V
mmonolayer water content [g H2O/100g d.m.],
Cconstant energy [kJmol
-1
].
The sorption properties research results were
developed using Microsoft Office Excel 365 computer
programs. The choice of the classic BET model was
determined by the recommendation of the
International Union of Pure and Applied Chemistry
(IUPAC) [32].
The fitting of empirical data to the BET equation
was characterised based on the value of determination
coefficient (r'), fitting of standard error (FitStdErr) and
statistics value F, calculated also using Jandel. Table
Curve 2D v 5.0,1 software [13].
In order to determine the suitability of the model
for the description of obtained adsorption isotherms,
analysis of the mean square error (RMS) expressed in
% was performed, which was calculated based on the
equation:
²
*100
ep
e
zw zw
zw
RMS
N



=
(2)
where:
zw
eexperimental activity, [g H2O/100g d.m.],
zw
pcomputed activity, [g H2O/100g d.m.],
Nthe observation number.
Based on the water content estimated in the
monolayer adsorbed at a temperature lower than the
boiling temperature and the so called water cross
section, the specific surface area of adsorbent was
calculated according to the equation (3) [22]:
(3)
where:
a
spsorption specific surface, [m
2
/g d.m.],
NAvogadro number, [6.023×1023 molecules /mol],
Mwater molecular weight, [18 g/mol];
ω – water setting surface, [ω = 1.05·10-
19
·m
2
/molecule].
3 RESULTS AND DISCUSSION
The determination of water content and activity are
the basic criteria for assessing the quality and
evaluation of products transported by sea. The level of
water content and activity of green coffee beans is
mostly influenced by the method of post-harvest
treatment of the grain, storage and transport
conditions. Green coffee beans, as tea leaves,
constitute very hygroscopic plant material and they
are very susceptible to water. During the green coffee
beans transportation process, the relative humidity of
the surrounding air could be increased, then beans of
coffee tend to absorb water. On the other hand, as the
relative humidity drops, green coffee beans tend to
desorb water. Very importent is also to along with
water sorption, the thermodynamic sorption
properties of the material should be monitored by
assessing the water activity (aw). According to
Baptestini et al. [1], the thermodynamic properties of
agricultural products is a key resource that can
provide information for assessing the effect of aw on
product storage and transportation and they can aid
in the understanding of the adsorbed water properties
and the study of physical phenomena that occur on
product surfaces. Table 1 presents the mean water
content and water activity of green bean coffee
samples.
Table 1. Corresponding water content and water activity
values for green bean coffee samples
_______________________________________________
Product Mean SD Water SD
water activity
content [-]
[g/100 g d.m.]
_______________________________________________
I (India) 9.8712 0.0003 0.6563 0.0015
II (India) 8.8775 0.0001 0.6218 0.0012
III (Ethiopia) 8.8795 0.0014 0.5797 0.0012
IV (Ethiopia) 8.8685 0.0003 0.5973 0.0037
V (India) 10.3785 0.0006 0.6876 0.0007
VI (Columbia) 10.6678 0.0010 0.6816 0.0003
VII (Guatemala) 8.3880 0.0007 0.5846 0.0027
_______________________________________________
Abbreviation: SD /standard deviation
Source: Own correlation (n=3).
Table 1 indicates that the obtained values of the
initial water content of all samples of coffee was
consistent with the literature data determining the
water content in coffee and did not exceed the
recommended content of 8-12% [10, 29]. Based on the
obtained results it can be assumed that the water
content was determined primarily by the country of
origin and different processing procedures. Despite
the water content in accordance with the ICO
standards, coffee beans from India (I, II and V), as
well as coffee beans from Columbia (VI), were
characterized by a high level of water activity, which
could indicate a relatively low degree of water
bonding with the dry matrix of green coffee beans raw
[20, 21, 24].
The high values of the initial water activity in all
green coffee samples could indicate low
microbiological stability of the tested products. The
probable reason for this was the adsorption of water
on the surface of coffee beans resulting from the
phenomenon of condensation occurring as a result of
the daily temperature fluctuation during sea
transport.
644
Moisture content can be the principal parameter
for assessing the current status of a coffee lot.
Transport of coffee can be considered as an extension
of storage of coffee but at the same time introduces
practical challenges in meeting the storage strictures
of avoidance of re-wetting and maintaining the
temperature on the constant level. Even well-dried
coffee contains a great deal of water that, as long as it
remains evenly distributed, poses no problem.
However, the fluctuations of temperature can cause
condensation and local re-wetting and lead to fungal
and their metabolites - toxins (especially Ochratoxin
A) outgrowth. According to ICO, Ochratoxin A is a
heat-stable mould metabolite produced by a few
species Aspergillus especially Aspergillus ochraceus,
which which develops in environments with
temperature ranged from 8 to 37
O
C with the optimum
temperature between 24 and 31
O
C. The minimum
water activity for its development amounts to 0.76 at
25
O
C, with the optimum aw between 0.95 and 0.99.
Although Aspergillus ochraceus develops from a
water activity of 0.76 then the optimal level of aw to
the toxins produced in green coffee beans is between
0.85, and 0.97. Ochratoxin A (OTA) can occur in raw
and roasted coffee beans. Additionally the toxins
produced by these fungi survive roasting and could
present a potential hazard for health. [8, 30].
Additionally, excess water can cause the
hydrolysis of some aroma compounds, the adverse
effects of oxygen, and polymerization of the aromatic
compounds contained in coffee.
The characteristics of the green coffee beans
hygroscopic properties were determined by
comparing the position of water vapour sorption
isotherms (Fig. 1). An sorption isotherm is a graphic
representation of the relationship between water mass
per dry matter and water activity in a constant
temperature and describes the state of dynamic
equilibrium of the system. Knowledge of the shape of
isotherm allows to evaluate the mechanism
determining the water binding process in the product,
identify the product sensitivity to moisture and
predict changes during the storage of product. Results
obtained from equilibrium moisture studies are
important for knowing how a material absorbs and
loses moisture during storage, and for defining the
transport conditions in order to maintain the best
quality of product [12, 31]. Sorption isotherms are also
efficient tools to determine thermodynamic
interactions between water and food components. [6,
17, 20].
Figure 1. The sorption isotherm of water vapor product I -
VII, determined after 30 days of storage in environment
with a
w= 0.07-0.98.
Source: Own correlation.
Sorption isotherms determined empirically in the
tested green coffee beans were characterized by
sigmoidal in shape and, the classification by Brunauer
showed similarity to the isotherms of type II. These
results are similar to those found by Dmowski and
Ruszkowska [4], Menkov [15, 16] and Pałacha and
Karwowski [23], working respectively with black tea
leaves (Camellia sinensis and assamica), lentils (Lens
esculenta), chickpeas (Cicer arietinum) and bean
(Phaseolus vulgaris).
The sigmoidal shape of the sorption isotherms is
related to the occurrence of the range of monolayer
adsorption in the low water activity (aw<0.3), the
multilayer adsorption range (0.3<aw<0.75) and the
capillary condensation area (aw>0.75). Developed
sorption isotherms in the tested coffee samples,
characterized by continuity in the course of the entire
range of water activity (0.07÷0.98) with increasing
water activity increased the water content in the
analyzed green coffee beans.
Based on the analysis of the course of empirically
determined isotherms, in the range of water activity
a
w = 0.07÷0.55, in green coffee beans from India (II),
Ethiopia (III and IV) and Guatemala (VII), water
desorption process was found, while above the range
of environmental water activity an adsorption process
was found.
It can be assumed that such a course of desorption
and adsorption process in the tested green coffees was
determined primarily by the water content in the
tested products and its state related to the chemical
composition of products.
In wet-processed green coffee beans from India (I)
and Colombia (VI) and dry-processed coffee from
India (V), characterized by a high initial water content
and water activity (Table 1), the desorption process
involved monomolecular sorption (a
w=0.07÷0.33) and
the multilayer sorption range (a
w=0.44÷0.75) (Fig. 1).
After exceeding the water activity a
w=0.75, in all tested
samples of green coffee beans I-VII, significant
intensification of the adsorption phenomenon was
found, expressed by an increase in the rate of water
vapour absorption process, which indicated the
initiation of capillary condensation. This phenomenon
can be equated with exceeding the level of critical
moisture, which determines the loss of product's
ability to be stored further [20].
By comparing the course of sorption curves in a
common frame of reference it was found that coffee
beans from India II (wet method production) had a
higher position, indicating greater hygroscopicity
(starting from water activity a
w=0.85). According to
the literature data, the course of sorption isotherms
could probably be affected by the diverse chemical
composition of the IVI products, but above all by
their structure (Fig. 1). When assessing the sorptive
properties of lyophilized strawberries, Ciurzyńska
and Lenart [3], found that they have a sigmoidal
shape characteristic of most food products,
corresponding to type II isotherms. In turn, Moraga,
Martinez-Navarrete and Chiralt [18] for freeze-dried
strawberries obtained a sorption isotherm course
typical of products with high sugar content. Probably,
it is connected with the slow changes in equilibrium
645
water contents at low water activity and rapid
increase of water activity above 0.5.
In order to determine the selected parameters of
surface microstructure, the empirical data was
subjected to the use of the Brunauer, Emmett and
Teller equation BET (1). The course of sorption
isotherms in the water activity range from 0.07 to 0.33
enabled to determine the parameters of BET equation
(vm, ce) by assaying the degree of its fit (R2, RMS,
SKO) to empirical data. The results were presented in
Table 3.
According to the literature data, the mean square
error (RMS) is lower than 10% and this indicates a
good agreement of the model fit to the data in the
studied range of water activity [20, 23]. Based on the
research, it was found that the calculated RMS in
green coffee beans I-VI ranged from 3.66% to 9.04%.
This confirmed that the parameters of the BET model
mathematically properly describe the process of water
vapor sorption on the surface of evaluated green
coffee beans. Only in the case of green coffee beans
from Guatemala (VII), the RMS value exceeded 10% -
indicating a smaller fit of the model.
Monolayer capacity (vm) determined based on the
BET equation, corresponds to a single layer of
molecules adsorbed water vapour and is referred to as
an indicator of the availability of polar water vapour
independently, the component of which is a source of
hydrophilic groups [14]. Theoretically, the water
content of the layer corresponds with the optimum
amount of water in the product and indicates the
quality of the storage and transport stability. The
monolayer moisture content is the safest moisture
content for storage and transport purposes, because at
a certain temperature it provides the increased time
period with minimum quality loss. Values below
monolayer moisture content slow down the
respiration rate of the product and the action of pests
[6]. On the other hand, the excess of water in relation
to the monomolecular layer leads to achieving the
critical humidity, the excess level of which may cause
undesirable changes in the product, especially the
development of microorganisms and toxins produced
by fungi (OTA), that are very dangerous. [8, 14, 19,
26].
The determined values of monolayer v
m range
from 3.06 g H
2O/100g for coffee originated from India
to 4.77 g H
2O/100g for coffee from Guatemala (Table
3). The obtained results showed that a greater surface
area of sorption was characterized by the Guatemalan
coffee processed by wet method, thus coffee from this
region was characterized by the highest storage and
transport stability.
According to Babtestini et al. [1] the C constant is
associated with the chemical potential differences
between the monolayer and superior layers. Constant
energy gives information about the difference
between the enthalpy of desorption monolayer and
the enthalpy of vaporization of the liquid adsorbent.
The results of constant Ce (Ce 2) confirm the
sigmoidal shape of the curve of adsorption and
suggest that in the tested products only a process of
physical adsorption was observed [27]. The lowest
value of constant Ce was characteristic of the coffee
from Guatemala, which indicated a lower amount of
heat released from the product in the sorption
process.
The determined values of monolayer capacity (vm)
based on the BET model constituted grounds for the
calculation of the sorption specific surface (Table 1).
The highest value of monolayer capacity based on the
BET model was determined in coffee from Guatemala
(VII) 167.7468 m
2
/g, and the smallest in coffee
from India (II) 107.6927 m
2
/g. Thus, it is possible
to assume that the highest stability and storage
stability determined by the value of monomolecular
layer, was characteristic of the samples from
Guatemala (VII). Based on the obtained results, it can
be assumed that the differences in the microstructure
of the product surface were determined by the
different treatment process parameters used by the
producers of the tested products and a different raw
material composition of the tested green coffee beans.
It can also be assumed that the process of
technological processing as well as the process of
transporting products by sea caused changes in the
structure of the evaluated green coffee beans.
Probably the products imported from India (I, II, V),
Ethiopia (III, IV) and Colombia (VI) were
characterized by a smaller number of active sites
capable of attaching water molecules. According to
Ocieczek [21] and Ruszkowska [25] the size of
sorption specific surface is the product of total surface
area and its affinity for water molecules determined
by the distribution of functional groups.
The research also included the measurement of
water activity of green coffee beans, performed after
30 days of storage in hygrostats with constant relative
humidity covering the range of water activity between
0.07 and 0.98 (Fig 2.).
Table 3. BET equation parameters and specific surface of sorption [m
2
/g]
__________________________________________________________________________________________________
Product vm [gH2O/100g] ce R
2
RMS [%] SKO Specific surface of sorption [m
2
/g]
__________________________________________________________________________________________________
I (Indie) 3.6806 8.7084 0.9944 8,5062 1,1668 129.3134
II (Indie) 3.0652 27.0375 0.8110 3,6630 1,3673 107.6927
III (Ethiopia) 3.9922 9.5233 1.0000 9,0408 1,4655 140.2632
IV (Ethiopia) 3.6904 11.5388 0.9971 4,7529 0,8982 129.6601
V (Indie) 3.5597 10.7666 0.9973 5,7973 1,0111 125.0669
VI (Columbia) 3.5918 11.6868 0.9974 8,5602 1,2313 126.1958
VII (Guatemala) 4.7745 4.7595 0.8778 28.5784 1,9110 167.7468
__________________________________________________________________________________________________
Abbreviation: R
2
- determination coefficient; FitStdErr - standard error; SKO sum of squared deviations
Source: Own correlation.
646
Figure 2. Water activity of I - VII green coffee, determined
after 30 days of storage in the range of a
w from 0.07 to 0.98,
at 20°C.
Source: Own correlation.
Fig. 2 provides that the greatest differences
between environmental water activity and water
activity measured in green coffee beans were
observed in the environment with water activity
(a
w=0.75÷0.98). Adsorption processes dominated in
this range of water activity. It was found that the time
of storage and possible transport of raw materials
were too short for the investigated raw materials to
reach a state of equilibrium in higher environmental
water activities.
Evaluation of the analyzed parameters is of
fundamental importance to the correct transportation
of the product, providing necessary information to
design the climatic conditions such as temperature or
relative humidity.
4 CONCLUSIONS
1 1. Under the obtained results, it can be concluded
that the examined green coffees, despite having a
similar initial water content in line with the Code
of Practice guidelines, were characterized by a
high level of initial water activity.
2 2. High water activity in the green coffee beans
imported to Poland by sea from India (I, II and V),
as well as coffee from Colombia, may indicate the
process of mouldy grains and thus contribute to
the formation of Ochratoxin A (OTA).
3 3. Assessing the quality and transport durability of
green coffee beans, based on the parameters of the
monomolecular layer capacity and the specific
surface area of sorption, it was found that coffee
imported from India (II) was the least susceptible
to changes in the transport conditions.
4 4. Taking into consideration the quality, storage
and transport stability of the tested green coffee
beans, the coffees processed by wet method,
imported from Guatemala (VII) and Ethiopia (III)
have had the best sorption properties. These were
the samples with the highest monomolecular layer
capacity.
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