Soil changes in a subtropical seasonal forest chronosequences in the south of Brazil/Mudancas no solo em cronossequencias da floresta estacional subtropical no sul do Brasil.
The scientific literature brings many studies on the changes in the physical, chemical, and biological properties of soils after deforestation (GUARIGUATA & OSTERTAG, 2001; MOJIRI et al., 2011) and in medium and long times of crops cultivation (HUGGETT, 1998; SCHOENHOLTZ et al., 2000; YEMEFACK et al., 2006). After the field crop abandonment, usually due losses in soil fertility, the forest succession starts, where soils remain protected against erosion and surface runoff while a new system nutrient accumulation/cycling through the vegetation takes place (GUARIGUATA & OSTERTAG, 2001). There is a controversy on the development of new soils after disturbances whether it occurs in a progressive (stable or non-self-organized) or in an unstable way (chaotic or self-organized) (HUGGETT, 1998).The study method of chronosequences assumes that sites under similar environmental conditions but, with different ages, can indicate sequences of ecosystem development after disturbances. Due to the advantages of low cost and rapid data collection, this method has been used to test theories on secondary succession on the vegetation (FRELICH, 1992; BARNES, et al., 1998) and on soils after disturbances (HUGGETT, 1998; AN et al., 2008).
The largest areas covered by remnant native forests in the state of Rio Grande do Sul, South of Brazil, are in the southern plateau edge (SPE) (CORDEIRO & RASENACK, 2009). Most of these areas are currently covered by secondary forests resulting from abandoned field crops, in different decades, over Leptosol and Regosol (PEDRON et al., 2010).
The objectives of this study were to answer the following questions: (1) Do different forest soils present specific features depending on the secondary forest age? (2) What are the best indicators for forest soils changes through the secondary succession? (3) Are the changes in forest soil properties linear towards time? These questions were approached through the evaluation of possible patterns in the chemical and grain size features of forest soils in 5 to more than 100-year-old chronosequences in the RSP using Fisher's discriminant models.
MATERIALS AND METHODS
The study forests are located in the central region of the southern edge plateau (SPE) in the state of Rio Grande do Sul, South of Brazil. The climate is Cfa, according to the Koppen classification, with an average annual temperature of 19.2[degrees]C, with the lowest and highest averages of 10.1[degrees]C and 27[degrees]C, respectively. The average annual rainfall is 1697.2 mm (INMET, 2009). The Leptpsols and Regosols in the upper slopes of the SPE are formed by volcanic rocks of the Serra Geral formation, and in the lower slopes were originated from sandy-quartzitic sediments of the formations of Botucatu and Caturrita. The leptosols frequently have a lithic contact, whichis a layer of unaltered rock in a depth of 50 cm from the surface. In the regosols, the lytic contact occurs a depth greater than 50cm (PEDRON et al. 2009; 2010).
The dominant vegetation in these scarps is the subtropical seasonal forest (SPICHIGER et al., 2000). The study areas are in a strip of land with a low variability in climate, geology, and vegetation whether compared to the whole SPE forest cover. Details on the composition and structure of the vegetation in each of the sampled areas are described by KILCA (unpublished data).
The decision on which areas should be sampled were based on the recommendations of FRELICH (2002): interviews with landowners and old dwellers (to know the kind of disturbance and the land use history), recent and old satellite imagery on the chosen areas (Google Earth and aerial photography from 1960 to 1970), floristic composition (presence of indicator species), and the vegetation structure (size). The four chronosequencies were represented by forests with different ages (5 up to > 100 years) that regenerated from the abandonment of field crops and maintained with no anthropic disturbances. Furthermore, forests with different ages were adjacent in each chronosequence and in similar positions in the SPE (Table 1). Therefore, the influences of different environmental variables were minimized in the sampling. After this, the results have less errors than a single random sample.
The identification of contacts between soils, saprolite and rock was done through the cutting shovel test (PEDRON et al., 2009). Given the pedologic variety in SPE environments, soils having at least 80% of their area in the same soil class were classified as belonging to the class.
In all the stands, 1000-[m.sup.2] plots split in 10 sub-plots of 10m*10m were established. This plot size is enough to represent the vegetation features and to reduce the scale-dependence of the physic and biological variables of the study in both space and time scales (HUGGETT, 1998; FRELICH, 2002).
Inside each 10m*10m sub-plot three compound samples of top soil (0-15cm in depth) were collected to determine the chemical and grain size composition. The basic cations ([Ca.sup.2+], [Mg.sup.2+], [K.sup.+], [Na.sup.+]), the potential acidity ([H.sup.+] + [Al.sup.3+]), the exchangeable [Al.sup.3+], N, pH, and the organic matter were determined. The cation exchange capacity, the sum of bases, and the base saturation were calculated according to the method recommended by EMBRAPA (1997). The grain size composition was assessed through the pipette method, according to EMBRAPA (1997).
To evaluate in what extend the soils variables can contribute to determine the ages of forest soils, Fisher's discriminant analisys was used (FDA). The FDA is a predictive multivariate analysis used to separate or characterize groups (non-metric variables) through several independent metric variables (BROWN & WICKER, 2000; MANLY, 2005). The FDA was run considering the following model assumptions: a) mutually exclusive groups (forests with different ages), b) satisfactory forest size (minimum number of 10 cases per groups), c) low correlation among variable (according to the Pearson's correlation test), d) dat normality (Kolmogorov-Smirnov's test), and the homogeneity of the covariance matrixes (test M of Box) (BROWN & WICKER, 2000). After applying these tests, the variables were not standardized to construct the discriminant model (MANLY, 2005).
The final data matrix was built with 250 cases (collections on the sub-units), 25 groups (ages of the forest soils), and 17 independent variables (soil features). The variable selection to be used in the model was determined by the test Wilk's Lamda (X) and the stepwise method to include variables in the model. The variable was included in the Fisher's discriminant method when the F value had the significant level of P<0.05 and when P>0.10 the variable was removed from the model (BROWN & WICKER, 2000). The probability of a case to belong to a given group was calculated through the lowest value of the Mahalanobis' distance (MANLY, 2005).
The four Fisher's discriminant models (FDMs) had high eingenvalues and high accumulated variances, not only for the two discriminant functions (DFs) (Table 2), but for the three DFs (VF - 88%, PS - 96%, no QCSP - 91%, and IMBR - 100%, nonpresented data). The FDMs also showed high canonic correlation values for each DF (Table 2).
Three chronosequences (VF, PS, and IMBR) had high values (>90%) of correct classifications of the soil features in the forest ages, where QCSP had the lowest correct classification (80%) (Table 3). Sixteen forest soils presented specific features related to a given forest age (100% of the cases correctly classified). Most of the plots had a strong correspondence with forest age versus soil features (from 80 to 90% of the sub-plots correctly classified) and a few areas with divergencies (60 and 70% sub-units correctly classified) (Table 3).
Not all the 14 variables included in the FDMs were able to distinguish soils of different forest ages. The models suggested different numbers of soil variables for each chronosequence (VF and PS - nine, QCSP - eight, and IMBR- four) to distinguish forest ages (Table 2). Weight correlations of each variable in each FDM (Table 2) showed the soil features that could be considered as good indicators of soil changes towards the forest succession. Two variables (N% and clay %) were presented in the four chronosequences and the variables of grain size had the largest contribution for the FDMs (except in QCSP) (Table 2). The two-dimensional maps of the four FDMs showed a non-regular distribution of the forest ages towards the two ordination axes, with no trends of linear changes of the soil features through the succession (Figure 1 A-D).
The FDMs showed that different soil chemical and grain size features were sufficient to distinguish significantly the forest soil ages in the four chronosequences of the SPE. The efficiency of the FDMs was similar to studies using the same statistic technique to differing chemical and physical properties of the soil in different environmental conditions (ZHANG et al., 2006; ASTEL, 2008; YE & WRIGHT, 2010). The biggest soil classification errors in the different forest ages were observed in the QCSP forests, in the region with the longest time of intensive and diversified soil use (>40 years alternating pastures and agriculture) in relation to other chronosequencies.The intensive soil use alters the soil properties, including its capacity to retain mineral nutrients (BARNES et al., 2008).
The FDMs of this study mostly showed that fertile Leptosols and Regosols can change their characteristics along time with the vegetation succession. Attributes related to soil fertility (basic cations--Ca, Mg, and K and N%, C%) and the soil grain size (clay, silt, and sand) characterized the forest soils ages. Attributes of the soil fertility are strongly altered under agricultural use of soils, they are good indicators of the soil quality (SCHOEBENHOLTZ et al., 2000; NORTCLIFF, 2002; AN et al., 2008). In the SPE, secondary forests over slopes with ages of 35, 55, and 90 years showed an increasing nutrients accumulation on the soil through litter (N>Ca>K>Mg) (BRUN et al., 2011). This natural condition of nutrients increasing and the great floristic variability in different forest ages (KILCA, unpublished data) shows how difficult is to rank soil indicators in common for all chronosequences. Moreover, less evident factors that also interfere on the soil chemical and grain size changes through the forest succession need to be considered in the analyses. They can be related to mineralogical variations of the volcanic rocks in the relief (PEDRON et al., 2009; 2010) and the historical soil use of each site (BARNES et al., 1998) as well as small scale natural variability of the soils (NORTCLIFF, 2002). The variables pH, Na, Al e Al% were not firstly included in the FDMs due to their low variabillity in the ANOVA tests and their weak importance on differing leptosols and regosols. A few features evaluated separately showed the tendency of increasing towards the increase of abandonment time (KILCA, unpublished data).
The study method of chronosequences has been efficient to describe the pedogenetic evolution of the soil in time scales from a few to thousands of years. This study, however, did not show the soil evolutionary direction during decades of vegetation development. So, it is not in accordance with the more traditional theory on the soil formation, where the soil evolves up to reach a balance with the environmental conditions (HUGGETT, 1998). The results of this study better fit in the theory of a pedogenetic evolution, where random environmental events promote an unpredictable sequence of soil development. Non-linearity of the process is related to the environmental conditions (due to exchanges, permanent additions, losses, tranfers, and changes in the enviromental substances).
This study showed that eutrophic's leptosols and regosols can present features significantly different towards one decade of forest development. However the soils features change in a non-linear way through the forest succession. This turns more difficult predictions of specific indicators shared by different soils due to the structure and floristic variation during the vegetation dynamics and other scale-dependent factors. Permanent studies on soil dynamics in the same forest area could improve the predictability of the changes in indicators just in a small scale.
This study was part of the PhD thesis of the first author. The research activities were funded by the "Programa Universal" of Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) (n. 477409/2010-5) while his fellowship was granted by Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES). The authors are very grateful to SEMARS (Dra. Suzane B. Marcuzzo and Felipe K. Rangel), CORSANRS (Mr. Roberto B. Cavalheiro), and Mr. Vanderlei Mezzomo ([cruz]) to permit data collection in their properties. The authors also acknowledge the very useful suggestions given by three reviewers.
AN, S. et al. Soil quality degradation processes along a deforestation chronosequence in the Ziwuling area, China. Catena, v.75, p.248-256, 2008. Available from: <http://naldc.nal.usda.gov/naldc/ download.xhtml?id=27011&content=PDF>. Accessed: Nov. 14, 2013. doi: 10.1016/j.catena.2008.07.003.
ASTEL, A., et al. Effect of environmental conditions on chemical profile of stream water in sanctuary forest area. Water, Air and Soil Pollution, v.195, p.137-149, 2008. Available from: <http:// link.springer.com/article/10.1007%2Fs11270-008-9733-9>. Accessed: Jan. 14, 2012. doi: 10.1007/S11270-008-9733-9.
BARNES, B.V. et al. Forest ecology. 4.ed. New York: John Wiley & Sons, 1998. 774p.
BROWN, M.T.; WICKER, L.R. Discriminant analysis. In: TINSLEY H.E.A.; BROWN, S.D. (Eds.). Handbook of applied multivariate statistics and mathematical modelin. San Diego: Academic, 2000. p.209-234.
BRUN, E.J. et al. Aspecto da ciclagem do material organico e nutrientes da serapilheira. In: SCHUMACHER, M.V. et al. (Orgs.). A floresta estacional subtropical: caracterizacao e ecologia no rebordo do Planalto Meridional. Santa Maria: Palloti, 2011. p.195-213.
CORDEIRO, J.L.P.; HASENACK, H. Cobertura vegetal atual do Rio Grande do Sul. In: PILLAR, V.D. et al. (Eds.). Campos sulinos: conservacao e uso sustentavel da biodiversidade. Brasilia: Ministerio do Meio Ambiente, 2009. p.285-299.
EMBRAPA (EMPRESA BRASILEIRA DE PESQUISA AGROPECUARIA). Manual de metodos de analises de solo. 2.ed. Rio de Janeiro: Ministerio da Agricultura e do Abastecimento, 1997. 212p.
FRELICH, L.E. Forest dynamics and disturbance regimes: studies from temperate evergreen-deciduous forest. Cambridge: Cambridge University, 2002. 280p.
GUARIGUATA, M.R.; OSTERTAG, R. Neotropical secondary forest succession: chances in structural and functional characteristics. Forest Ecology and Management, v.148, p.185-206, 2001. Available from: <http://lerf.eco.br/img/ publicacoes/2001_3011%20Neotropical%20secondary%20 forest%20succesion.pdf>. Accessed: Dec. 14, 2010. PII: S03781127(00) 00535-1.
HUGGETT, R.J. Soil chronosequences, soil development, and soil evolution: a critical review. Catena, v.32, p.155-172, 1998. Available from: <http://www.sciencedirect.com/ science/article/ pii/S0341816298000538>. Accessed: Dec. 15, 2010. PII: S03418162(98)000 53-8.
INMET (INSTITUTO NACIONAL DE METEOROLOGIA). Normais climatologicas do Brasil 1961-1990. RAMOS, A.M. et al. (Orgs.) Brasilia, DF: INMET, 2009. 465p.
MANLY, B.F.J. Multivariate statistical methods: a Primer. 3.ed. Boca Raton: Chapman & Hall, 2005. 214p.
MOJIRI, A. et al. Effects of land use changes on soil quality attributes (a review). Research Journal of Agriculture and Biological Sciences, v.7, n.11, p.1-3, 2011. Available from: <http://www.aensiweb.com/ old/rjabs/rjabs/2011/1-3.pdf>. Accessed: Dec. 06, 2013.
NORTCLIFF, S. Standardization of soil quality attributes. Agriculture, Ecosystems and Environment, v.88. p. 161-168, 2002. Available from: <http://www.researchgate.net/profile/ Stephen_Nortcliff/publication/223516232_Standardisation_of_ soil_quality_attributes/links/0912f5063127801b7a000000.pdf>. Accessed: Dec. 06, 2013. PII: S0167-8809(01)00253-5.
PEDRON, F. de A. et al. Morfologia e classificacao taxonomica de Neossolos e saprolitos derivados de rochas vulcanicas da Formacao Serra Geral no Rio Grande no Sul. Revista Brasileira de Ciencia do Solo, v.33, p.119-128, 2009. Available from: <http://www.scielo.br/readcube/epdf.php?doi=10.1590 /S010006832009000100013&pid=S0100-06832009000100013&pdf_ path=rbcs/v33n1/13.pdf>. Accessed: Nov. 10, 2013. doi: 10.1590/ S0100-06832009000100013.
PEDRON, F. de A. et al. Morfologia dos contatos entre solosaprolito-rocha em Neossolos derivados de arenitos da Formacao Caturrita no Rio Grande do Sul. Revista Brasileira de Ciencia do Solo, v.34, p.1941-1950, 2010. Available from: <http://www.scielo. br/scielo.php?pid=S0100-06832010000600019&script=sci_ arttext>. Accessed: Nov. 10, 2013. doi: 10.1590/S0100 06832010000600019.
SCHOENHOLTZ, S.H. A review of chemical and physical properties as indicators of forest soil quality: challenges and opportunities. Forest Ecology and Management, v.138, p.335-356, 2000. Available from: <http://soilslab.cfr.washington.edu/ ESRM410/WhatIf3/ Schoenholtz-etal-2000.pdf>. Accessed: Nov. 10, 2013. PII: S 0378-1127(00)00423-0.
SPICHIGER, R. et al. Geographical zonation in the Neotropical of tree species characteristic of the Paraguay-Parana basin. Journal of Biogeography, v.31, p.1489-1501, 2000. Available from: <http:// onlinelibrary.wiley.com/doi/10.1111/j.1365-2699.2004.01071.x/ full>. Accessed: Oct. 10, 2010. doi: 10.1111/j.1365 2699.2004.01071.x
YEMEFACK, M. et al. Empirical modelling of soil dynamics along a chronosequence of shifting cultivation systems in southern Cameroon. Geoderma, v.133, p.380-397, 2006. Available from: <http://www.sciencedirect.com/science/journal/00167061/133>. Accessed: Oct. 10, 2010. doi: 10.1016/jgeoderma.2005.08.003.
YE, R.; WRIGHT, A.L. Multivariate analysis of chemical and microbial properties in histosols as influenced by land-use types. Soil & Tillage Research, v.110, p.94-100, 2010. Available from: <http://www.sciencedirect.com/science/journal/01671987/110/1>. Accessed: Sep. 13, 2013. doi: 10.1016/j.still.2010.06.013.
ZHANG, C.B. et al. Characterization of soil physico-chemical and microbial parameters after vegetation near ShaoguanPb/Zn Smelter, Guangdong, p.r. China. Water, Air, and Soil Pollution, v.177, p. 81-101, 2006. Available from: <http://link.springer.com/ article/10.1007/s11270-006-9096-z>. Accessed: Sep. 13, 2013. doi: 10.1007/s11270-006-9096-z.
Ricardo de Vargas Kilca (I) Fabricio de Araujo Pedron (II) Gustavo Schwartz (III) Solon Jonas Longhi (IV) Gabriel Antonio Deobald (II)
(I) Programa de Pos-graduacao (CAPES-PNPD), Laboratorio de Dendrologia e Fitossociologia, Centro Agroveterinario (CAV), Universidade do Estado de Santa Catarina (UDESC), 88520-000, Lages, SC, Brasil. E-mail: firstname.lastname@example.org. Corresponding author.
(II) Departamento de Solos, Centro de Ciencias Rurais (CCR), Universidade Federal de Santa Maria (UFSM), Santa Maria, RS, Brasil.
(III) Embrapa, Unidade Amazonia Oriental, Belem, PA, Brasil.
(IV) Programa de Pos-graduacao em Engenharia Florestal, CCR, UFSM, Santa Maria, RS, Brasil.
Returned by the author 07.28.15
Table 1--Forest chronosequences analyzed in the central region of southern plateau edge (SPE) in Rio Grande do Sul, South of Brazil. Areas/ages Soil class Rock Surface VF VF-15 LepE Ba Slopes VF-25 RegE Ba/San Slopes VF-35 RegE Ba Slopes VF-70 LepE Ba Slopes VF-MF1 LepE Ba Slopes VF-MF2 LepE Ba Slopes PS PS-15 LepE Ba Slopes PS-25 LepE Ba Slopes PS-40 LepE Ba Slopes PS-50 LepE Ba Slopes PS-60 LepE Ba Slopes PS-90 RegE Ba Slopes QCSP QCSP-5 LepE Ba Plane QCSP-10 LepE Ba Plane QCSP-15 RegE Ba Plane QCSP-30 LepE Ba Slopes QCSP-50 LepE Ba Slopes QCSP-60 LepE Ba Slopes QCSP-90 LepE Ba Slopes QCSP-MF LepE Ba Slopes IMBR IMBR-30 LepE Ba Slopes IMBR-60 LepE Ba Slopes IMBR-80 LepE Ba Slopes Areas/ages Land use Declivity Coordinates22J VF VF-15 SA H 248035/6719392 VF-25 SA U 247913/6719443 VF-35 SA SU 247846/6719378 VF-70 SA H 248123/6719389 VF-MF1 NO H 247541/6719643 VF-MF2 H 248530/6719398 PS PS-15 SA GU 295282/6717618 PS-25 SA SU 295181/6717673 PS-40 SA SU 295241/6717280 PS-50 SA H 295295/6717002 PS-60 SA H 295211/6717684 PS-90 SA H 295355/6717129 QCSP QCSP-5 SA U 278610/6738795 QCSP-10 SA GU 278584/6739377 QCSP-15 SA GU 278843/6738382 QCSP-30 SA H 279060/6738195 QCSP-50 SA H 279210/6738325 QCSP-60 SA H 279201/6738361 QCSP-90 SL H 278122/6739287 QCSP-MF NU H 278893/6738820 IMBR IMBR-30 SA H 227390/6728454 IMBR-60 SA H 227259/6728567 IMBR-80 SL H 226968/6727813 VF--Silveira Martins municipality; PS- Paraiso do Sul municipality; QCSP- Quarta Colonia State Park, Agudo municipality; and IMBR (Ibicui Mirim Biological Reserve) Itaara municipality. MF--Mature forest, >100 years old over dense rock outcrops (1) and over a few rock outcrops (2). Rock: Sa (Sandstone), Ba (Basaltic). Soil classes: LepE--Leptosol eutrophic, RegE- Regosol eutrophic. Surface morphology of the SPE according to PEDRON et al. (2010). Land use: SA- smallholder agriculture, SL- selective logging, NO- forest with no use. Declivity: gently undulating (GU) 3-8%; undulated (U) 8-20; strongly unulating(SU) 20-45%; hilly (H) 45-75%. Table 2--Results of the four Fisher's discriminant models for the soil features in four forests chronosequences of the southern edge plateau, state of Rio Grande do Sul, Brazil. VF PS Discriminant Functions Variables 1 2 1 2 Eingenvalues 9.0 3.1 53.3 5.6 % variation 59.2 20.7 80.3 8.5 % acum. var. 59.2 79.9 80.3 88.9 Can. cor. 0.94 0.87 88.9 0.92 Features 1 2 1 2 Ca -0.23 -0.03 -- -- Mg -- -- 0.02 -0.13 K 0.22 0.40 0.06 -0.26 H+Al 0.02 0.34 -- -- N (%) -- -- -0.05 0.19 C (%) -- -- -0.04 0.20 [CE.sub.Cef] -- -- 0.01 -0.35 [CEC.sub.pot] -- -- 0.04 -0.40 V (%) -- -- -0.02 -0.12 SB -0.18 0.03 -- -- Sand 0.77 -0.01 -- -- Clay -0.15 0.74 0.07 0.45 Silt -- -- 0.75 -0.09 QCSP IMBR Discriminant Functions Variables 1 2 1 2 Eingenvalues 5.8 3.4 5.1 2.7 % variation 51.9 30.1 65.1 34.9 % acum. var. 51.9 82.0 65.1 100.0 Can. cor. 0.92 0.88 0.91 0.85 Features 1 2 1 2 Ca -- -- -- -- Mg 0.09 0.02 -- -- K 0.73 0.03 -- -- H+Al 0.26 -0.55 -- -- N (%) 0.32 0.39 -0.21 0.04 C (%) -- -- -0.22 0.10 [CE.sub.Cef] -- -- -- -- [CEC.sub.pot] -- -- -- -- V (%) 0.15 0.43 -- -- SB 0.33 -0.01 -- -- Sand -- -- -0.60 0.20 Clay 0.37 -0.40 0.87 0.38 Silt -0.46 -0.01 -- -- Chronosequencies: VF--Silveira Martins; PS--Paraiso do Sul; QCSP-State Park of Quarta Colonia; BRIM--Biological Reserve of Ibicui Mirim.% acum. var.--Percentage of the accumulated variation; Can. cor.--Canonic correlation; CTCef.--Effective CEC; CTCpot.--Potential CEC. Table 3--Classification of the soil features of four forests chronosequences of the southern edge plateau, through the Fisher's discriminant analysis. Area % of Area % of classifications * classifications * VF QCSP A- VF15 100 A-QCSP8 100 B-VF25 90 (10 F) B-QCSP10 80 (20 F) C-VF35 100 C-QCSP15 60 (20 A; 20 D) D-VF60 100 D-QCSP30 70 (30 A) E-MF1 100 E-QCSP60 100 F-MF2 70 (30 D) F-QCSP70 90% (10 B) Total 93.3 G-QCSP90 60 (30 B; 20 F) H-MF 80 (10 D; 10 F) PS Total 80.0 A-PS15 100 IMBR B-PS25 100 A-IMBR30 90 (10 B) C-PS35 100 B-IMBR60 100 D-PS50 100 C-IMBR80 100 E-PS60 100 Total 96.7 F-PS80 90 (10 C) Total 98.3 * incorrect classifications and soil characterist similarity ().
|Printer friendly Cite/link Email Feedback|
|Title Annotation:||ciencia del suelo; texto en ingles|
|Author:||Kilca, Ricardo de Vargas; Pedron, Fabricio de Araujo; Schwartz, Gustavo; Longhi, Solon Jonas; Deobal|
|Date:||Dec 1, 2015|
|Previous Article:||Common bean elite lines cultivated under nitrogen fertilization and inoculation with Rhizobium tropici/Linhagens elite de feijoeiro-comum cultivadas...|
|Next Article:||Growth and yield of two common bean cultivars as affected by 2,3,5-triiodobenzoic acid rates/Crescimento e produtividade de duas cultivares de feijao...|