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Spatial variability of soil fertility and its relation with cocoa yield/ Variabilidade espacial da fertilidade do solo e sua relacao com a produtividade do cacaueiro.


In the last years, the southern portion of the Bahia state, the main cocoa-producing region of Brazil, has faced a serious production crisis, due to the appearance and spread of the witch-broom disease (Souza Junior et al., 2011). With the diffusion of new tolerant seminal and clonal varieties, this problem has been slightly solved with the gradual recovery of production (Arevalo et al., 2007).

However, cocoa production sustainability is related, besides more efficient genetic materials, to the utilization of specific production systems including the use of correctives and fertilizers (Chepote et al., 2013). In this context, the knowledge on the variability of soil fertility and determination of fertilizer doses to be applied constitute a decisive step for the cocoa crop management.

The increase in the efficiency of agricultural managements must contemplate the spatial and temporal variability existing at the field (Silva et al., 2015). Thus, it is possible to optimize the use of agricultural inputs with reduction of economic and environmental risks, obtaining greater profitability and quality of the products (Corwin & Lesch, 2003).

Given the above, this study aimed to evaluate the spatial variability of soil fertility and its relation with coca yield.

Material and Methods

The study was conducted over 14 months from 2014 to 2015, in a 0.6-ha area of the Cocoa Research Center- CEPEC/ CEPLAC, located in the municipality of Ilheus-BA, Brazil, at latitude (14[degrees] 47' S; 39[degrees] 16' W). The soil was classified as eutroferric Haplic Nitosol, according to the Brazilian Soil Classification System (EMBRAPA, 2013).

The experimental area was implemented in 2003 with 31 cocoa progenies in the agroforestry system with shade of Erythrinas. Cocoa has been cultivated at spacing of 3.0 x 1.5 m and Erythrina at spacing of 24 x 24 m.

The sampling for the determination of soil chemical characteristics and crop yield was performed in a sampling grid with 120 points referenced using the local coordinate system. Soil collection was performed in November 2014, under the cocoa canopy projection at a distance of 0.50 m from the stem, in the layer of 0-0.20 m. Four subsamples (one per quadrant) were used to form a composite sample per sampling point.

The soil samples were sent to the laboratory for the evaluation of chemical attributes: phosphorus (P), potassium (K), calcium (Ca), magnesium (Mg), sulfur (S), sodium (Na), iron (Fe), boron (B), copper (Cu), manganese (Mn), zinc (Zn), aluminum (Al), active acidity (pH in water), potential acidity (H + Al) and calculation of sum of exchangeable bases (SB), potential cation exchange capacity [CEC at pH 7 (T)], including the base saturation index (V%), Al saturation index (m%) and the remaining phosphorus (P-rem). Soil analyses followed the methodologies presented by EMBRAPA (2011).

The production was monthly evaluated from July 2014 to November 2015 and stratified in off-season cocoa (March to August), season cocoa (September to February) and annual production (sum of all months). The total healthy fruits in each sampling point and the dry weight of seeds per fruit were determined. The results were converted to yield (kg [ha.sup.-1]) using the spacing of the crop.

The data were initially subjected to descriptive statistical analysis. Normality was evaluated by the Shapiro-Wilk (W) test at 0.05 probability level. Pearson's coefficient was used to evaluate the existence of correlation between the data of soil chemical attributes and cocoa yield.

Subsequently, geostatistical analysis was applied to verify and quantify the spatial dependence, through the fit of experimental variograms, according to Eq.1:

[??](h) = 1/2N(h) [2(h).summation over (i=1)] [Z([x.sub.i])-Z[([x.sub.i] + h).sup.2]] (1)


[gamma](h)--semivariance estimated using the experimental data; and,

N(h)--number of pairs of observations Z([x.sub.i), Z([x.sub.i + h), separated by a vector h.

The models tested for the fit of theoretical functions to the experimental variograms were spherical, exponential, Gaussian and linear with plateau. Models with higher value of R2 (coefficient of determination), lower RSS (residual sum of squares) and higher value of correlation coefficient given by the cross validation were selected.

The degree of spatial dependence (DSD) was determined using the relationship [C.sub.0]/([C.sub.0] + C) and the classification proposed by Cambardella et al. (1994). After confirming the spatial dependence, the data were interpolated through ordinary kriging (Isaaks & Srivastava, 1989), to estimate values in non-sampled sites.

The maps interpolated for each chemical attribute were subjected to a fuzzy classification system, to establish the pertinence of the pixels to a certain standard set, according to Silva et al. (2010). The standard set for each soil chemical attribute was established based on the manual of recommendation of fertilization for cocoa (Chepote et al., 2013). A linear fuzzy model was used, in which higher values are equal to the standard, considered as equal to 1, while the lower values are modeled to determine their pertinence to the referred set. In the case of H + Al, high values are harmful; thus, the inverted linear model was used.

The combined effect of the attributes was measured using map algebra functions through the weighted average fuzzy operator. Equal weight was attributed to all representations, i.e., it was considered that the attributes contributed equally in the estimation of soil fertility (Silva et al., 2010).

Results and Discussion

The descriptive statistics for the analyzed variables are presented in Table 1. The attributes Al, Na and m (%) are not shown in the table, because the values were equal to zero for all sampling points. The values of mean and median, except for P and cocoa yield, were similar for all attributes. According to Cambardella et al. (1994), this can be an indication that the central tendency measurements are not dominated by atypical values in the distribution.

The mean values found for P (> 16 mg [dm.sup.-3]), K (> 10 [cmol.sub.c] [dm.sup.-3]), Mn (> 9.0 mg [dm.sup.-3]), Fe (> 30 mg [dm.sup.-3]) and Zn (> 1.5 mg [dm.sup.-3]) were high (Chepote et al., 2013). The values of H + Al (< 5 [cmol.sub.c] [dm.sup.-3]), potential CEC (> 8 [cmol.sub.c] [dm.sup.-3]), V (> 40%), Ca (> 5 [cmol.sub.c] [dm.sup.-3]), SB (> 5 [cmol.sub.c] [dm.sup.-3]), OM (> 1.5 dag [cm.sup.-3]), S (> 10 mg [dm.sup.-3]), Cu (> 1.2 (mg [dm.sup.-3]) and pH are within the limits established as adequate. On the other hand, the attributes Mg (< 1.9 [cmol.sub.c] [dm.sup.-3]) and B (< 0.9 mg [dm.sup.-3]) remained below the recommended values for the cocoa crop.

Souza Junior et al. (1999) comment that a good cocoa yield results from the balance between the nutrients of the soil. According to these authors, soils that are rich in micronutrients tend to be more productive, provided that these elements do not reach toxic levels. Cidin et al. (2009), studying fertility in a soil under agroforestry system composed of cocoa and coconut trees, observed mean values of pH, P and K of5.3, 2.3 mg [dm.sup.-3] and 0.23 [cmol.sub.c] [dm.sup.-3], respectively. Silva Junior et al. (2012), analyzing a soil cultivated with agroforestry system composed of cocoa and 'cupuacu', obtained mean values of pH, P and K of 4, 9.8 mg [dm.sup.-3] and 0.06 [cmol.sub.c] [dm.sup.-3], respectively, which is much lower than the values found in the present study.

The mean yields of off-season, season and annual cocoa were 1322, 393 and 1865 kg [ha.sup.-1], respectively. Season cocoa represents the main production of the crop; however, in this study the off-season cocoa showed higher yield, and the result is due to the genetic variability between the cocoa trees and the soil conditions, which allowed in this period an increase in the number of fruits and dry weight of seeds per fruit. Evaluating cocoa yield in different periods, Souza Junior et al. (1999) observed that the mean yield of the three most productive years varied from 1447 to 2675 kg [ha.sup.-1].

The coefficients of variation were low (CV% < 12) for pH, Ca, Mg, SB, CEC (T) and V (%), medium (CV% [greater than or equal to] 12 and [less than or equal to] 60) for K, P, P-rem, OM, S, Zn, B, Cu, Fe, Mn, H+Al, and high (CV% > 60) for the yield of season, off-season and annual cocoa, according to Warrick & Nielsen (1980). The coefficient of variation is a measure of dispersion employed to estimate the precision of experiments (Mohallem et al., 2008) and is a good indication of the variability existing in a data set.

The CV values of the yield of off-season, season and annual cocoa were 75.6, 93 and 78%, respectively, indicating high variability. Such behavior can be attributed to the genetic variability among the progenies cultivated in the area and to the variation of soil chemical attributes, based on the correlation analysis presented in Table 2. Leite et al. (2012) found CV of 44% for potential yield of two clones of cocoa and 60% for the effective yield.

According to Table 2, the stratifications of cocoa yield showed negative and significant linear correlation with the potential CEC of the soil. This value is different from those reported in the literature and can be attributed to the high variability observed for the yield of the crop. Silva et al. (2015) comment that correlations between variables with different variabilities (different CVs) may not be explanatory, indicating the need of analyses that consider the spatial distribution pattern.

The behavior observed for yield in relation to CEC (T) can also be related to factors associated with the type of soil in study. Since part of the CEC (T) is occupied by potential acidity, it is possible to claim that in regions of lower availability of nutrients the effect of acidity is more evident, influencing crop yield. The effect of potential acidity tends to be greater in soils with lower contents of clay, compromising yield (Pegoraro et al., 2008).

Mattioni et al. (2013) and Souza et al. (2010) observed negative linear correlation between CEC (T) and yields of soybean and sugarcane, respectively. Although the abovementioned studies used crops other than cocoa, it becomes evident the possibility of negative correlations between yield and the potential CEC of the soil.

Similar behavior was observed for the yields of season and annual cocoa, for OM and B levels, which can be justified by the reduced levels of both in the soil, as previously discussed.

According to the geostatistical analysis (Table 3), all attributes, except Mg, show spatial variability in the studied area and fitted to variograms with well-defined plateaus. The theoretical models that best fitted to the experimental variograms were spherical, exponential and Gaussian.

The degree of spatial dependence (DSD) of the attributes was moderate for pH, K, V, CEC (T), Ca, OM, S, Zn, B, Cu, Fe, Mn, H + Al and off-season cocoa, and strong for P, SB, P-rem, fertility, season and annual cocoa, according to Cambardella et al. (1994). These results indicate that, except for CEC (DSD > 50%), the higher proportion of data variability can be attributed to the space that separates the samples, and the random component is less predominant. Higher DSD values improve the estimation through ordinary kriging, facilitating the interpretation of the phenomena (Isaaks & Srivastava, 1989).

The map of yield for off-season cocoa (Figure 1) indicates that a large extension of the area has yield between 0 and 8500 kg [ha.sup.-1], with a small part of the area reaching up to 12000 kg [ha.sup.-1]. Season cocoa showed yield lower than 3000 kg [ha.sup.-1] while annual yield reached 12500 kg [ha.sup.-1]. Genetic and environmental factors may interfere with the yield of a plant (Leite et al., 2012), as well as factors related to the adopted management (Silva et al., 2010). In the case of cocoa, besides these factors, the cultivation in agroforestry systems allows different results for yield. Thus, the variation expressed inside and between systems suffers influence from those existing in the soil, plant and in the covering canopy (Deheuvels et al., 2012).

Soil fertility, integrated by the fuzzy classification system, showed high variability in the studied area (Figure 1), suggesting that fertilizers and correctives must be applied considering such variation. In general, the soil has medium to high possibility of production for the cocoa crop, because the pertinence values of fertility based on the weighting of the individualized attributes are within the interval of 0.48 to 0.98.

The western region of the area showed the lowest fertility levels, with pertinences below 0.68. This same region showed the lowest values of pH, SB and V and the highest values of H+Al, indicating that they can be the most limiting variables to cocoa yield in the studied area. The other attributes also show lower values in this portion of the area, but they are mostly above the levels considered as desirable for cocoa production.

Cocoa yield showed significant spatial correlation at 0.05 probability level with soil fertility. However, the relationship between the yield of season and the fertility was low ([R.sup.2] = 36%; y = -0.0029 + 0.2298*x) and, in this case, the preponderant effect on yield variability is due to factors other than the availability of nutrients, such as genetic or environmental factors.

The yield of off-season cocoa and the annual yield showed spatial correlation of 59% (y = -0.3399+0.8209*x) and 53% (y = -0.1646 + 0.4713*x) with soil fertility, respectively, indicating that the greatest proportion (> 50%) of the spatial variability of yield in these periods can be associated with soil fertility. Although the correlation analysis does not provide precise information on cause and effect, it is possible to claim that, for off-season cocoa, fertility was decisive to increase the number of fruits and the dry weight of seeds per fruit, increasing the yield in the period.

The annual yield is obtained by the sum of season and off-season; hence, the correlation is justified by the result observed for this last period, since it was on average about four times higher compared with the season. Souza Junior et al. (1999) comment that the highest yields are expected in the season, but it is possible to claim, based on the results of the present study, that with high levels of soil fertility the yield of off-season cocoa can be equally high or higher.

The results of the present study indicate that, when a cocoa production system is studied based on the spatial analysis and no longer in average terms, various pieces of information not yet evidenced start to be observed. Studies like this can lead to more efficient management interventions, which result in the achievement of higher crop yield.


1. The use of geostatistics allowed to identify specific regions with variable levels of the attributes, which can be used as reference for the correction of soil fertility in variable rates.

2. The soil of the area, except for the western region, showed possibilities from medium to high for the cocoa cultivation.

3. Soil fertility exhibited positive spatial correlation with cocoa yield, and its effect is preponderant only for off-season and annual cocoa.



The authors thank the National Council for Scientific and Technological Development (CNPq) for the financial support to the research.

Literature Cited

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Warrick, A. W; Nielsen, D. R. Spatial variability of soil physical properties in the field. In: Hillel, D. (ed.). Applications of soil physics. New York: Academic Press, 1980. p.319-344. https://doi. org/10.1016/B978-0-12-348580-9.50018-3

Railton O. dos Santos (1), Lais B. Franco (1), Samuel A. Silva (2), George A. Sodre (3) & Agna A. Menezes (4)

(1) Universidade Estadual de Santa Cruz/Programa de Pos-Graduacao em Producao Vegetal. Ilheus, BA. E-mail:;

(2) Universidade Federal do Espirito Santo/Centro de Ciencias Agrarias e Engenharias/Departamento de Engenharia Rural. Alegre, ES. E-mail: (Corresponding author)

(3) Comissao Executiva do Plano da Lavoura Cacaueira/Centro de Pesquisa do Cacau. Ilheus, BA. E-mail:

(4) Universidade Estadual de Santa Cruz/Departamento de Ciencias Agrarias e Ambientais. Ilheus, BA. E-mail:

Ref. 026-2016--Received 9 Mar, 2016 * Accepted 11 Nov, 2016 * Published 5 Jan, 2017

Caption: Figure 1. Maps of yield distribution of off-season cocoa, season cocoa and annual production and soil fertility integrated by the fuzzy classification system
Table 1. Descriptive statistics and frequency distribution of soil
attributes and cocoa yield

Attribute       Mean       Median        SD       CV (%)     Maximum

pH              6.30        6.30        0.15       2.40       6.70
K               42.20       41.50       14.2      32.10       82.00
P               38.50       32.50       22.0      57.10       67.80
Ca              7.30        7.40        0.88      11.90       9.10
Mg              1.90        1.90        0.11       5.64       2.10
H + Al          2.20        2.30        0.88      40.10       2.80
SB              9.36        9.38        0.91       9.76       10.90
CEC (T)         11.50       11.60       0.40       3.50       12.60
P-rem           24.20       24.90       4.0       16.50       31.60
OM              4.13        4.10        0.5       12.06       5.20
S               21.20       21.00       4.68      22.05       33.0
Zn              2.83        2.90        0.89      31.46       5.10
B               0.81        0.83        0.12      14.16       1.03
Cu              2.68        2.70        0.98      36.70       4.90
Fe              82.20       84.00       16.9      20.60      111.00
Mn              88.40       89.00       23.2      26.20      127.00
Off-season     1322.00     1073.00      999       75.60      3828.00
Season         393.00      327.00      365.5      93.00      1438.00
Annual         1865.00     1449.00      1463      78.00      6350.00

Attribute     Minimum      Cs        Ck       w

pH              6.10      0.17      -0.99    (ns)
K              26.00      0.83      -0.29    (ns)
P               7.90      0.18      -1.64    (ns)
Ca              5.80      -0.05     -1.12    (ns)
Mg              1.70      0.12      -0.55    (ns)
H + Al          0.70      0.04      -1.13    (ns)
SB              7.68      -0.09     -1.11    (ns)
CEC (T)        10.80      0.31      -0.12    (ns)
P-rem          15.50      -0.19     -1.12    (ns)
OM              3.30      0.44      -0.63    (ns)
S              10.00      0.39      -0.12    (ns)
Zn              1.10      0.28      -0.30     *
B               0.50      -0.38     -0.14     *
Cu              0.40      -0.20     -0.02     *
Fe             37.00      -0.41     -0.43    (ns)
Mn             25.90      -0.17     -0.52    (ns)
Off-season      0.00      0.58      -0.70    (ns)
Season          0.00      0.93      0.13     (ns)
Annual          0.00      0.82      0.03     (ns)

SD--Standard deviation; CV--Coefficient of variation; Cs--Coefficient
of asymmetry; Ck--Coefficient of kurtosis; w *--Non-normal distribution
by the Shapiro Wilk test at 0.05 probability level; w (ns)--Normal
distribution; Ca, Mg, H + Al, Na, SB, CEC (T)--cmolc [dm.sup.-3]; K, R
Fe, Zn, Cu, Mn, S, B--mg [dm.sup.-3]; P-rem--mg [L.sup.-1]; OM--dag
[cm.sup.-3]; V--Base saturation (%); pH ([H.sub.2]O), Al (1 mol
[L.sup.-1] KCl); P and K (Mehlich-1); Ca and Mg (1 mol [L.sup.-1]
KCl); Fe, Zn, Cu and Mn (Mehlich-1); OM (oxidoreduction); S (MCPa); B
(hot water); P-rem (0.01 mol [L.sup.-1] Ca[Cl.sub.2])

Table 2. Correlation (n = 120) between soil attributes and
yield (season, off-season and annual)

Attributes     Season    Off-season     Annual

pH             0.07      -0.11         -0.06
K             -0.02      -0.05         -0.05
P             -0.10      -0.09         -0.11
Ca             0.04      -0.13         -0.09
Mg            -0.03      -0.18         -0.15
H+Al          -0.16       0.06         -0.01
SB             0.04      -0.15         -0.11
CEC (T)       -0.48 *    -0.43 *       -0.48 *
V              0.14      -0.07         -0.01
P-rem         -0.01      -0.04         -0.04
OM            -0.44 *    -0.15         -0.40 *
S              0.04       0.06          0.06
Zn             0.17       0.20          0.41 *
B             -0.41 *    -0.16         -0.43 *
Cu            -0.41 *    -0.09         -0.15
Fe             0.10       0.15          0.15
Mn             0.02       0.02          0.02

* Significant at 0.05 probability level

Table 3. Models and parameters of the variograms fitted to soil
attributes and cocoa yield

Attribute    Model    [C.sub.0]    [C.sub.0] +    RSS    [R.sup.2]

pH            EXP        0.38         1.06       0.01      0.925
K             SPH        0.47         1.17       0.71      0.961
P             SPH        0.29         1.53       0.27      0.993
Ca            EXP        0.35         1.05       0.01      0.935
Mg            PNE         --           --         --         --
H+Al          SPH        0.46         1.03       0.00      0.933
SB            EXP        0.20         1.04       0.01      0.953
CEC (T)       GAU        0.77         1.25       0.01      0.925
V             SPH        0.44         1.04       0.14      0.977
P-rem         GAU        0.34         1.92       0.38      0.995
OM            SPH        0.54         1.20       0.01      0.965
S             EXP        0.35         1.01       0.11      0.795
Zn            EXP        0.31         1.30       0.02      0.958
B             SPH        0.55         1.22       0.00      0.961
Cu            SPH        0.46         1.19       0.06      0.887
Fe            SPH        0.56         1.13       0.10      0.671
Mn            EXP        0.43         1.05       0.48      0.900
Season        SPH        0.16         0.96       1.73      0.897
Off-season    SPH        0.50         1.00       2.15      0.653
Annual        SPH        0.02         1.01       1.38      0.899
Fertility     SPH        0.12         0.97       0.15      0.866

Attribute     DSD    Range (m)    [R.sup.2]    SE Pred

pH           35.9        35         0.341        0.17
K            40.0        70         0.473        0.12
P            19.0       107         0.610        0.08
Ca           33.9        30         0.356        0.17
Mg            --         --           --          --
H+Al         44.4        22         0.407        0.13
SB           19.0        25         0.260        0.20
CEC (T)      55.0        90         0.215        0.21
V            42.0        30         0.303        0.17
P-rem        18.0       108         0.621        0.08
OM           44.5        84         0.388        0.14
S            34.9        30         0.299        0.17
Zn           24.0       100         0.482        0.12
B            45.0        81         0.353        0.17
Cu           38.5        72         0.379        0.14
Fe           49.0        68         0.395        0.13
Mn           40.0        32         0.377        0.15
Season       16.9        12         0.267        0.20
Off-season   45.0        15         0.294        0.19
Annual       2.20        18         0.392        0.14
Fertility    12.4        13         0.338        0.17

[C.sub.0]--Nugget effect; [C.sub.0] + C--Sill; RSS--Residual sum of
squares; [R.sup.2]--Coefficient of determination of the model; DSD--
Degree of spatial dependence; [R.sup.2](CV)--Coefficient of
determination of the cross validation; SE Pred--Percent error of the
estimate; EXP--Exponential; SPH--Spherical; GAU--Gaussian; PNE--Pure
nugget effect
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Author:dos Santos, Railton O.; Franco, Lais B.; Silva, Samuel A.; Sodre, George A.; Menezes, Agna A.
Publication:Revista Brasileira de Engenharia Agricola e Ambiental
Article Type:Ensayo
Date:Feb 1, 2017
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