geographical discrimination of honeys by using mineral composition and common chemical quality...
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Geographical discrimination of honeys by usingmineral composition and common chemicalquality parametersAna M Gonzalez Paramas,1 J Alfonso Gomez Barez,1 Rafael J Garcia-Villanova,1*Teresa Rivas Pala,1 Ramon Ardanuy Albajar2 and Jose Sanchez Sanchez3
1Departamento de Quımica Analıtica, Nutricion y Bromatologıa, Facultad de Farmacia, Universidad de Salamanca, Campus ‘Miguel deUnamuno’, E-37007 Salamanca, Spain2Departamento de Estadıstica, Facultad de Ciencias, Universidad de Salamanca, Salamanca, Spain3Departamento de Botanica, Facultad de Biologıa, Universidad de Salamanca, Salamanca, Spain
Abstract: Sixty honey samples from six different production zones of the provinces of Salamanca,
Zamora and CaÂceres (western Spain) were analysed for 13 common legal physicochemical parameters
and 17 mineral elements (13 cations and four anions) in order to test for their geographical
classi®cation. Application of linear stepwise discriminant analysis to a number of variables made of a
selection of analytical results and their simple mathematical functions allowed, ®rstly, discrimination
between honeys from all six zones and, secondly, discrimination between honeys from the three zones
of the province of Salamanca. The most discriminant variables selected for the six zones were 10 in
number, a combination of three physicochemical parameters and nine elements, with a result of
91.38% of correctly classi®ed samples; for the three zones of the province of Salamanca, regarded with
special interest in our study, six variables were selected (made of eight elements) with a result of 97.07%
of correctly classi®ed samples.
# 2000 Society of Chemical Industry
Keywords: honey mineral composition; honey legal physicochemical parameters; honey geographical origin;linear discriminant analysis
INTRODUCTIONThe honey market currently shows a tendency to
production and hence characterisation of honeys as
either uni- or multi¯oral, thus providing the consumer
with a wide variety of choice. Furthermore, there is a
tendency to establish geographical limits of production
with the aim of protecting a production zone that has
developed and marketed a particular standard of
quality. Each of these circumstances has speeded up
the establishment of procedures during recent years
for the determination of either the botanical or the
geographical origin.
Regarding the botanical origin, microscopical
examination of the sediment (melissopalynological
analysis) was the ®rst technique to be used and,
currently complemented by sensory analysis, con-
tinues to be a reference tool for this purpose. However,
its known limitations have encouraged the search for
physicochemical parameters or, more directly, speci®c
chemical compounds that, as such or as a result of
transformation, could be used as unequivocal indica-
tors of botanical origin. Although no single or small
number of parameters has yet been reported to be
exclusive to each kind of uni¯oral honey, there are a
few compounds or parameters proposed as de®nitive
markers: methyl anthranilate1 or the ¯avonoid
hesperetin2 for citrus honeys and the norisoprenoid
S-dehydrovomifoliol3 for heather honeys. In the
absence of a single clear parameter, many authors
have tested statistical methods using a correlation
matrix made up of a number of parameters determined
over a consistent number of samples. Krauze and
Zalewski4 used principal component analysis for 18
physical and chemical parameters over 88 honey
samples divided into four groups (acacia, rape,
linden�multi¯oral and honeydew), obtaining the
strongest associations for the values of electrical con-
ductivity, ash, free acids and proline. Mateo et al5
employed colour, as measured by two methods, for the
characterisation of Spanish uni¯oral honeys rosemary,
orange blossom, lavender, sun¯ower, eucalyptus,
heather and honeydew); by using discriminant analy-
sis, they achieved levels of correctly classi®ed samples
of 70.1% and 76.0% for the two methods. The same
Journal of the Science of Food and Agriculture J Sci Food Agric 80:157±165 (2000)
* Correspondence to: Rafael J Garcia-Villanova, Departamento de Quımica Analıtica, Nutricion y Bromatologıa, Facultad de Farmacia,Universidad de Salamanca, Campus ‘Miguel de Unamuno’, E-37007 Salamanca, SpainContract/grant sponsor: Spanish Government (CICYT); contract/grant number: ALI95-0715Contract/grant sponsor: Junta de Castilla y Leon (Regional Government); contract/grant number: 54/08/92(Received 4 May 1999; revised version received 29 July 1999; accepted 26 August 1999)
# 2000 Society of Chemical Industry. J Sci Food Agric 0022±5142/2000/$17.50 157
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honeys were later tested6 by discriminant analysis with
15 parameters, of which the following were selected by
the multivariate program as the most discriminantÐ
electrical conductivity, colour, water content, fructose
and sucroseÐwith an average level of correctly
classi®ed samples of 95.7%.
Regarding the determination of the geographical
origin of honeys, few references can be found in the
scienti®c literature. Two articles dealing with ¯avo-
noids in Portuguese heather honey7 and Tunisian
honeys8 reported different patterns of ¯avonoids with
respect to Spanish honeys, but without any further
systematic study. In contrast, three articles applied
multivariate analysis to a number of common chemical
parameters (legal quality indicators), sometimes in-
cluding a few sugars, with the aim of differentiating
their production areas in Spain: Sancho et al9 reported
differentiation of honeys from the three provinces of
the Basque Country with the help of a discriminant
mathematical function which selected ®ve variables
(total acidity, formol index, sucrose, fructose/glucose
and glucose±water/fructose ratios), with 77.4% of
correctly classi®ed samples; PenÄa and Herrero10
reported discrimination of honeys from two provinces
of Galicia (90% correct classi®cation) with the help of
only two common parameters (free acidity and
moisture content); ®nally, Sanz et al11 reported dis-
crimination of honeys from mountain and valley areas
of La Rioja (83% correct classi®cation) with four
parameters (ash content, conductivity, lactonic acidity
and fructose/glucose ratio). In most cases the authors
interpreted these results in terms of different ¯oral
origin.
Mineral composition has also been employed for the
purpose of geographical origin discrimination. The
mineral content of honey re¯ects the presence of
speci®c minerals within the forage area of the
hive.12±14 Varju15 determined the P, Ca, Mg, B, Cu,
Mn, Zn, Sn, Pb and total mineral contents of
Hungarian acacia honeys and reported a relationship
with those of plants and soils. An excess or insuf®-
ciency of certain chemical elements in soils, rocks or
water, as well as other phytosociological, environ-
mental or seasonal factors, is re¯ected in the mineral
composition of the plants and hence in the nectar,
pollen or honeydew.16,17 Taking this as a basis, Morse
and Lisk18 studied the elemental composition and
found signi®cant differences between honeys from the
United States, Mexico, El Salvador and China. Feller-
Demalsy et al19 undertook an ambitious trial to
differentiate honeys from the 10 Canadian provinces
by application of principal component analysis to the
data of 20mineral elements, achieving 92% correct
classi®cation; they found that these differences were
independent of the ¯oral origin of the honeys and
seemed to be very complexÐprobably they were
related to maritime in¯uence coupled with extent of
precipitation rather than being dependent upon soil
composition. Finally, Sauri and HernaÂndez20 applied
discriminant analysis to differentiate honeys of two
regions of Mexico by means of seven elements, with
100% correct classi®cation.
The contribution of contamination from the proces-
sing equipment and containers should also be con-
sidered. Acidic foods such as honey which had been in
contact with stainless steel surfaces during harvesting,
processing and/or preparation for market showed
higher values for Cr than those of comb honey, while
values for Ni did not re¯ect signi®cant variations.21
Honey contamination with Zn was also suggested to
occur via galvanised steel equipment.22
The present work is part of a wider study on the
quality of honeys from three zones of the province of
Salamanca (Fig 1) and of assays for their typi®cation
for a denomination of quality, as established in the
legislation of the European Union.23 These three
zones have an important production of honey from
wild vegetation almost without crops and of great
Figure 1. Geographical zones of honeyproduction studied.
158 J Sci Food Agric 80:157±165 (2000)
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biodiversity. Close to them are found three other
zones, also honey producers, on the borders of
Salamanca and with which bulk commercial ex-
changes are frequent. The objectives of this study
were: ®rstly, to determine whether it would be possible
to differentiate between honeys of all six zones to
establish geographical limits to the production of each;
secondly, to determine whether it would be possible to
differentiate between the three zones of the province of
Salamanca, geographically and botanically different,
and thus establish within it three distinct types/
qualities. This has been attempted by applying dis-
criminant analysis to the values obtained for physico-
chemical parameters established in the Spanish
Norma de Calidad24 and for mineral content.
EXPERIMENTALHoney samplesSixty samples of fresh bulk honey were collected
between 1992 and 1994, from beekeepers or research
hives of our group, in six geographical zones of the
provinces of Salamanca, Zamora and Caceres (Fig 1).
All the data of interest (location, date, extraction
procedure, heat treatment if any, temperature and
storage location, as well as botanical and climatologi-
cal data of the location of the hives) were recorded.
Given that the intention was to study in greater depth
the honeys of the province of Salamanca, 12 samples
were taken from each of its zones and only eight
samples from those of the rest. Melissopalynological
analysis revealed the botanical origin, and the results
are summarised in Table 1. The number of samples of
honeys from nectar, honeydew and `forest' (naturally
mixed nectar and honeydew honey) re¯ects approxi-
mately the proportion of each type of them produced
in each zone.
Chemical analysisThe 13 physicochemical parameters presented in the
Spanish Norma de Calidad for honey destined for the
home market24 were determined using the methods of
analysis25 summarised in Table 2. Seventeen mineral
elements were determined (13 cations and four
anions) by heating 15g of honey at 550°C, dissolving
the resulting ash in 10ml of a mixture of equal parts of
HCl (2M) and HNO3 (2M) and ®nally making the
solution up to 100ml with doubly distilled water. The
methods of analysis of the mineral elements are
summarised in Table 3.
The precision of each method was determined in the
range of average concentration to decide upon its
acceptability; for the metallic elements the detection
limit was also determined according to the criteria of
Kaiser26 (Tables 2 and 3).
Multivariate analysisLinear discriminant analysis, which utilises functions
of linear classi®cation with the statistical variables
employed (functions of classi®cation of Fisher27), was
applied. A function of classi®cation exists for each of
the groups, and each sample was assigned to the group
for whose function of classi®cation it had maximum
value. The coef®cients of the functions of classi®cation
were estimated from samples previously assigned to
groups by us, and the selection of the statistical
variables most adequate for classi®cation was carried
out by a sequential process. The statistical criteria used
to introduce and eliminate variables were based on the
entry and output probabilities (PIN and POUT); only
Table 1. Zones of honey production studied and botanical origin
Number of samples
Zone Total Nectara Honeydew Forest
1. Arribes del Duero 12 11 (1) ± 1
2. Sierra de Francia 12 1 2 9
3. Sierra de Gata 12 7 (2) 3 2
4. Sanabria 8 5 (5) ± 3
5. La Vera 8 5 (2) 1 2
6. Plasencia 8 7 1 ±
a Number of mono¯orals in parentheses.
Table 2. Common physicochemical parameters determined, methods and repeatability
Parameter Method
Coef®cient of variation
(%)
Proline Reaction with ninhydrin and colorimetry 3.0
Reducing sugars Redox volumetry of Fehling reagent with methylene blue end-point detection 0.29
Apparent sucrose As above, acid hydrolysis and subtraction of reducing sugars value 4.6
pH Glass electrode potentiometry 0.41
Free acidity Acid±base titration to pH=8.5 1.38
Lactonic acidity Acid±base titration to pH=8.3 3.40
Total acidity Summation of above two 1.15
Ash Heating at 550°C 4.5
Moisture Refractometry at 20°C 0.55
Hydroxymethylfurfural (HMF) Spectrophotometry at 284 and 336nm 5.40
Diastase number Gothe index 2.5
Electrical conductivity Conductimetry of 200g lÿ1 (DM) honey solution at 20°C 0.80
Insoluble matter Gravimetry after 20±40mm sieve ®ltration 8.5
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variables with P<0.05 (high discrimatory capacity)
were introduced in the equations. For this the program
SPSS Release 4.0, version for Macintosh, was used.
With regard to the size of the sample, the following
criterion was applied to ®x in the matrix of correlation
the number of variables (v) employed, as a function of
that of the samples (n) and the groups (g) into which
these are classi®ed:
v � �n=2� ÿ 2g ÿ 1
In turn, since in each group the employment of the
averages and variances of all the variables can be of
interest, the following condition should be ful®lled:
ngv � 4�v� v� � 8v
where ng is the number of samples per group, ie
ng � 8
RESULTS AND DISCUSSIONThe repeatability of each analytical method was ®rst
established in order to test the suitability of every
datum for this study; Tables 2 and 3 show that in
general the values of repeatability (% coef®cient of
variation) are acceptable, although some parameters
were ®nally rejected.
In Tables 4 and 5 the average values and ranges of
the common physicochemical parameters and mineral
elements respectively for each of the six geographical
zones studied are presented. Regarding mineral
composition, important differences can be observed,
especially within groups (ie within each of the six
zones) for some major elements such as Na and K,
which exceeded 100% of the coef®cient of variation
(CV) in the La Vera and Sierra de Francia zones
respectively. Among the minor elements, Al, Cd, Co,
Cr, Fe, Mn and Ni also exceeded 100% of the CV in at
least one of the six zones for each element. The
remainder of the elements presented less variability
within groups; in particular, the anions rarely exceeded
50% of the CV.
Discriminant analysis could now use the data of
these 13 physicochemical parameters and 17 mineral
elements determined to attempt to differentiate the six
or three geographical zones which were the object of
study (60 or 36 samples respectively), which would
entail a total of 30 variables. To these could be added
mathematical functions of the variables in case they
might yield more information and thus increase the
discriminant power of the function of classi®cation. It
was decided to choose the simplest function: a
quotient of two physicochemical parameters (lactonic
acidity/free acidity quotient, previously used by
Crane28) and the quotients of the mineral elements
that were quanti®able in all the samples. The following
considerations were made to establish the ®nal
number of variables.
(a) The parameters of moisture content, hydroxy-
methylfurfural, diastatic activity and insoluble
solids should not be considered representative of
the nature of the honey, but are rather indicators
of its adequate manipulation and freshness.
Furthermore, the last three have very high values
of repeatability (Table 2).
(b) Cd was found to have values which were
extremely high in three samples (see Table 5),
giving a clear indication of contamination,
probably from the processing equipment.
(c) By convention, the 0.5 detection limit was
adopted for those samples in which Co was not
quanti®able.
(d) Only the ratios of the quanti®able heavy metals
in all the samples were used, rather than those of
all the elements, because the former presented
the greatest variability among all the samples, as
Table 3. Analytical methods for mineral elements
Parameter Method Coef®cient of variation (%) Detection limit (mgkgÿ1)
Sodium Flame emission photometry 4.13 33
Potassium Flame emission photometry 8.73 6.40
Zinc Atomic absorption spectroscopy (¯ame) 6.31 0.04
Aluminium Atomic absorption spectroscopy (electrothermal) 2.35 6.70
Iron Atomic absorption spectroscopy (electrothermal) 3.15 10.0
Manganese Atomic absorption spectroscopy (electrothermal) 1.95 3.33
Copper Atomic absorption spectroscopy (electrothermal) 1.40 0.87
Chromium Atomic absorption spectroscopy (electrothermal) 7.65 3.73
Nickel Atomic absorption spectroscopy (electrothermal) 7.35 10.0
Cobalt Atomic absorption spectroscopy (electrothermal) 5.60 6.33
Cadmium Atomic absorption spectroscopy (electrothermal) 10.2 0.33
Calcium Complexometric volumetry 3.55 Ð
Magnesium Complexometric volumetry 8.34 Ð
Chloride Mercurimetric volumetry 0.58 Ð
Phosphorus Vanadomolybdate colorimetry of phosphate 0.60 Ð
Silicon Molybdene blue colorimetry of silicate 3.63 Ð
Sulphur Turbidimetry of barium sulphate 3.50 Ð
a mgkgÿ1.
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could be expected, thereby yielding greater
discriminant information. To some extent this
would be attributable to the different composi-
tions of the soils of the various zones and their
vegetation, without ignoring the contribution of
contamination from the processing equipment
or containers, a matter, though more disputable,
which could also constitute a differentiating
element.
The resulting list of variables used for characterisa-
tion is given in Table 6.
With regard to the number of samples, it was
decided to reject two from Sierra de Francia because
they had abnormally high values of heavy metals,
probably also due to contamination from the equip-
ment or containers, the number of samples thus being
reduced to 58.
Therefore the result is a total of 9�1�16�21=47
variables, which multiplied by 58 cases or samples
gives a matrix of correlation of 2726 data. In
accordance with the criteria selected in the multi-
variate analysis, it can be seen that the maximum
number of variables (v), as a function of the number of
groups (g) into which the samples (n) were to be
classi®ed, was as follows.
. In the case of classi®cation into the six geogra-
phical zones:
v � �58=2� ÿ �2� 6� ÿ 1 � 16 variables
Table 4. Results of common physicochemical parameters
Parameter Arribes del Duero Sierra de Francia Sierra de Gata La Vera Plasencia Sanabria
Proline (mgkgÿ1)
Mean 533 1029 833 659 836 863
Range 850±280 1600±690 1030±610 870±440 1080±450 1420±520
Reducing sugars (mgkgÿ1)
Mean 717.1 683.7 736.0 722.0 716.5 712.9
Range 755±655 714±653 779±650 759±677 763±667 758±637
Apparent sucrose (mgkgÿ1)
Mean 35.8 19.3 24.3 30.1 20.8 26.5
Range 91±10 35±3 50±10 72±15 42±7 43±11
Free acidity (meqkgÿ1)
Mean 24.53 44.94 36.19 33.36 30.93 34.35
Range 36.2±13.6 62.5±30.6 50.9±23.7 45.0±22.8 43.1±21.4 47.2±22.5
Lactonic acidity (meqkgÿ1)
Mean 6.33 5.76 5.66 5.96 6.49 3.66
Range 14.4±1.1 9.3±2.5 8.7±1.2 13.4±2.2 13.6±3.4 7.5±1.1
Lactonic acidity/free acidity
Mean 0.3053 0.1338 0.1673 0.1916 0.2368 0.1180
Range 0.662±0.030 0.261±0.054 0.317±0.040 0.515±0.060 0.636±0.111 0.333±0.027
pH
Mean 3.768 4.483 3.993 3.955 4.028 4.485
Range 4.27±3.38 4.98±3.97 5.03±3.20 4.47±3.41 4.57±3.58 4.76±4.31
Total acidity (meqkgÿ1)
Mean 30.88 50.73 41.85 39.33 37.41 38.01
Range 43.6±21.8 69.6±34.7 55.3±30.3 52.4±26.0 47.9±29.0 50.8±27.8
Moisture (gkgÿ1)
Mean 150.4 154.7 160.7 155.3 157.5 158.6
Range 176±138 175±135 178±145 166±138 175±140 173±149
HMF (mgkgÿ1)
Mean 14.03 3.43 9.53 21.49 14.26 2.08
Range 55.5±0.3 11.1±<0.3 29.3±0.4 68.1±0.7 30.1±<0.3 5.3±<0.3
Diastase number
Mean 21.90 55.17 32.37 31.40 31.88 35.48
Range 38.0±8.0 81.4±38.2 46.5±15.1 46.7±14.3 46.9±12.3 61.9±5.2
Electrical conductivity (mScmÿ1)
Mean 0.43 1.10 0.55 0.51 0.54 0.94
Range 1.1±0.2 1.4±0.8 1.1±0.3 0.9±0.2 1.1±0.2 1.3±0.6
Insoluble matter (gkgÿ1)
Mean 0.294 0.288 0.260 0.201 0.168 0.770
Range 0.59±0.043 0.57±0.12 1.0±0.055 0.45±0.094 0.56±0.023 4.5±0.044
Ash (gkgÿ1)
Mean 2.03 5.76 3.48 2.60 2.32 4.88
Range 5.9±0.45 7.2±4.3 8.2±1.7 5.7±0.88 5.7±0.45 6.2±3.4
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. In the case of classi®cation into the three zones of
the province of Salamanca:
v � �34=2� ÿ �2� 3� ÿ 1 � 10 variables
It can be seen that for both cases the number of
variables permitted was much smaller than the 47 in
the previous list. It was decided to reduce this number
as follows: ®rstly, by applying discriminant analysis
separately to the physicochemical parameters (10
variables) and then to the mineral elements and their
ratios (37 variables); secondly, by performing pre-
liminary exploratory analysis in case there was still an
excessive number of variables. Later, once a pre-
selection of the variables with greatest discriminant
power had been made, the maximum number permis-
Table 5. Results of mineral elements
Parameter Arribes del Duero Sierra de Francia Sierra de Gata La Vera Plasencia Sanabria
Na (mgkgÿ1)
Mean 55.8 118.9 84.9 121.1 74.1 70.1
Range 125±27 287±37 178±36 476±38 250±22 100±48
K (mgkgÿ1)
Mean 183.3 1483.8 440.5 736.8 453.3 779.0
Range 402±47 6785±514 677±180 1221±364 1172±90 1459±77
Ca (mgkgÿ1)
Mean 98.3 202.3 129.0 87.7 94.0 107.4
Range 172±60 420±107 236±66 125±59 212±51 165±62
Mg (mgkgÿ1)
Mean 23.9 78.1 56.7 54.1 54.7 63.8
Range 75±7 167±20 148±27 146±9 153±15 173±19
Al (mgkgÿ1)
Mean 3.04 5.30 5.31 6.04 3.11 8.31
Range 13±0.94 12±1.2 11±1.5 20±0.66 5.3±1.8 14±2.5
Fe (mgkgÿ1)
Mean 0.84 7.59 1.69 1.85 3.37 2.96
Range 1.5±0.60 60±0.71 2.8±1.0 2.7±1.2 5.3±0.92 4.2±0.80
Zn (mgkgÿ1)
Mean 1.25 1.99 1.66 2.57 2.76 1.19
Range 2.0±0.49 2.9±1.1 3.1±0.62 5.9±0.93 5.9±1.2 1.8±0.76
Mn (mgkgÿ1)
Mean 0.98 10.9 3.80 1.35 1.69 4.60
Range 2.6±0.42 45±3.4 9.3±0.82 3.2±0.36 3.3±0.36 13±1.9
Cu (mgkgÿ1)
Mean 361.3 1361.2 696.8 485.3 669.5 1325.3
Range 723±226 2300±547 1603±240 1066±217 1922±209 1988±961
Cr (mgkgÿ1)
Mean 56.3 843.3 55.1 94.5 50.1 54.0
Range 153±16 4480±49 94±19 225±17 142±14 78±35
Ni (mgkgÿ1)
Mean 121.0 747.3 186.6 49.9 130.5 146.5
Range 212±28 3373±137 900±33 76±29 288±10 296±33
Co (mgkgÿ1)
Mean 10.5 136.2 33.8 <DLa 4.1 8.3
Range 31±DL 720±15 219±DL DL±DL 11±DL 36±DL
Cd (mgkgÿ1)
Mean 3.6 5.6 24.1 54.2 2.7 50.2
Range 15±DL 15±DL 247±DL 355±DL 18±DL 274±0.57
Cl (mgkgÿ1)
Mean 181.3 307.3 338.0 244.4 317.6 427.2
Range 393±77 460±78 467±200 404±112 455±121 579±290
P (mgkgÿ1)
Mean 67.7 205.0 103.6 111.3 102.0 121.5
Range 134±36 350±78 169±62 189±57 213±47 207±59
S (mgkgÿ1)
Mean 27.8 53.8 52.0 39.6 38.6 30.0
Range 31±24 130±27 71±25 46±19 89±27 37±25
Si (mgkgÿ1)
Mean 21.7 18.7 18.9 18.0 11.5 38.1
Range 46.7±5.3 23.4±10.4 30.7±9.1 38.1±3.4 21.5±5.0 46.0±15.1
a DL, detection limit.
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sible would be introduced in each case (16 or 10
variables according to the case) and the de®nitive assay
would be carried out.
Discrimination between the six geographical zones(P=0.05)A ®rst assay, performed only with the variables of
physicochemical parameters, yielded the selection of
ash, proline and conductivity, achieving only 51.67%
of samples well classi®ed.
With the variables of mineral elements and their
ratios, ie 16�21=37 variables (v>16), the program
®rst carried out preliminary exploratory analysis and
pre-selected nine variables, which were later intro-
duced for the de®nitive assay. It selected then in the
order Cl, Mn/Al, Ni/Mn, Si, Fe, S, K, Cu and Ca, with
86.21% of samples well classi®ed.
An attempt to improve this percentage was made by
including the variables of physicochemical parameters,
ie 10�37=47 variables (v>16). The preliminary
exploratory analysis selected 10 variables (v<16),
which were those ®nally introduced, and the program
selected then in the following order.
1. Ash 36.21%
2. Proline 44.83%
3. Fe/Ni 56.90%
4. Cl 58.62%
5. Conductivity 68.97%
6. Cu 75.86%
7. Si 84.48%
8. S 89.66%
9. Ni/Mn 89.66%
10. P 91.38%
11. Mg 91.38%
The number of samples well classi®ed now rose
somewhat (91.38%), with equal discriminant power of
the variables S and Ni/Mn on the one hand and P and
Mg on the other. In Fig 2 the samples are classi®ed in
each zone with its centroid as a function of the values
of the ®rst two canonical functions. The numbers of
correctly/incorrectly classi®ed samples for each group
were: Arribes del Duero, 11/1; Sierra de Francia, 10/0;
Sierra de Gata, 12/0; La Vera, 8/0; Plasencia, 6/2; and
Sanabria, 6/2.
Discrimination between the three zones of theprovince of Salamanca (P=0.05)The assay carried out with only the 10 variables of
Table 6. List of variables employed for multivariateanalysis
Physico chemical parameters and ratios (10)
Mineral elements and
ratios (37)
Proline Lactonic acidity/free acidity Sodium Fe/Ni
Reducing sugars Potassium Fe/Zn
Apparent sucrose Zinc Fe/Cr
pH Aluminium Fe/Mn
Free acidity Iron Fe/Cu
Lactonic acidity Manganese Fe/Al
Total acidity Copper Ni/Zn
Ash Chromium Ni/Cr
Electrical conductivity Nickel Ni/Mn
Cobalt Ni/Cu
Calcium Ni/Al
Magnesium Zn/Cr
Chloride Zn/Mn
Phosphorus Zn/Cu
Silicon Zn/Al
Sulphur Cr/Mn
Cr/Cu
Cr/Al
Mn/Cu
Mn/Al
Cu/Al
Figure 2. Plot of canonical function 1 versus canonical function 2 with thesix centroids (* ) for the 58 samples.
J Sci Food Agric 80:157±165 (2000) 163
Geographical discrimination of honeys
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physicochemical parameters (v�10) achieved a high
number of samples well classi®ed (91.67%), selecting
four: total acidity, reducing sugars, conductivity and
ash.
With the variables of mineral elements and their
ratios, ie 16�21=37 variables (v>10), the program
®rst carried out a preliminary exploratory analysis and
pre-selected six variables, which were later introduced
for the de®nitive assay. It selected then in the order
Mn, Fe/Ni, Cr/Cu, Na, K and S, with 97.07% of
samples well classi®ed.
The conjunction of both types of variables did not
improve the percentage of classi®cation, though it
simpli®ed it, resulting in the following order.
1. Ash 61.78%
2. Total acidity 82.35%
3. Na 76.47%
4. Conductivity 91.18%
5. Cl 97.06%
In Fig 3 the samples are classi®ed in each zone with its
centroid as a function of the values of the ®rst two
canonical functions, and are separated into zones. The
numbers of correctly/incorrectly classi®ed samples for
each group were: Arribes del Duero, 12/0; Sierra de
Francia, 10/0; and Sierra de Gata, 11/1Ðie one
misclassi®ed sample out of 34.
CONCLUSIONSThe results of the study of the six honey-producing
zones demonstrate the poor discriminant power of the
physicochemical parameters (51.67% of samples well
classi®ed), while the variables elaborated with the
mineral elements considerably raise this value
(86.21%), and the conjunction of both classes of
variables raises it to 91.38%. Therefore the mineral
composition, presumably very dependent on the
soil15±17 and vegetation12±14Ðwithout neglecting con-
tamination from the processing equipment and con-
tainersÐhas a high power of differentiation of the
geographical origin in this case. The possible contam-
ination by heavy metals during harvesting, processing
and shipment was not studied, although the two
samples rejected because of very high values of Cd are
suspected of being subject to it. Should this occur, it
could be a contribution to the differentiation pattern of
the groups.
In the study of the three zones of the province of
Salamanca the discriminant power of the physico-
chemical parameters was much greater (91.67% of
samples correctly classi®ed), to which the smaller
number of groups of classi®cation undoubtedly con-
tributed. The variables made of mineral elements
achieve a greater value (97.07%, ie all the samples
except one), which also reveals a probable in¯uence of
the composition of the soil and its vegetation together
with possible contamination of the materials post-
harvest. The inclusion of all the parameters did not
improve the classi®cation (97.06%), but changed
notably the previously selected variables. This can be
explained in part by the distinct botanical origin of the
honeys in the three zones (Table 1): in Arribes del
Duero, those of nectar predominate, while in Sierra de
Gata and even more in Sierra de Francia, those of
forest or honeydew predominate. The pattern of
classi®cation is now rather that of the physicochemical
characteristics which, generally and a priori, are
attributed to one or the other: values of ash, con-
ductivity and macro-mineral content, greater in the
honeydew honeys than in those of nectar, which is
re¯ected in an unequivocal way by statistical analysis
as well.
ACKNOWLEDGEMENTSWe would like to thank Mr GH Jenkins for his
assistance with the English version of the MS. This
work was partly supported by the Spanish Govern-
ment (CICYT, ref ALI95-0715) and the Junta de
Castilla y LeoÂn (Regional Government, ref 54/08/92).
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