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Decomposition and release of nutrients from species of tropical green manure

ABSTRACT

Decomposition processes and mineralization are essential to determine the time to deploy and manage species in consortia or rotations. The aim of this article was study the dynamics of biomass decomposition and release of macronutrients of plant residues of Fabacea. The species used were: jack bean (Canavalia ensiformis), pigeon pea (Cajanus cajan), dwarf mucuna (Mucuna deeringiana) and sunn hemp (Crotalaria juncea). The experiment was conducted in the field in a randomized block design, 4 x 5 factorial, four species of green manure and five times (0, 30, 60, 90, and 120 days). In the results, sunn hemp and pigeon pea had lower decomposition and release of C, N, K, and Mg. All species, K and P showed similar half-lives (t1/2). For N, sunn hemp presented the lowest coefficient of mineralization (k), 0.0040 g g-1 dia-1, associated with highest t1/2 (173.3 days), already, jack bean showed the highest k (0.0122 g g-1 dia-1) associated with the lowest t1/2 (56.8 days). In edaphoclimatic conditions, use of the jack bean and the dwarf mucuna is recommended for supply of nutrients in shorter periods of time for subsequent crops. However, sunn hemp and pigeon pea are recommended for greater persistence of mulch on the soil.

Keywords
nutrient cycling; mineralization; Fabaceae

INTRODUCTION

In agricultural and natural systems, the processes of decomposition and nutrient release from organic residues added in the soil are controlled by three main factors: (1) physical-chemical conditions of the environment, which are controlled by the climate and soil characteristics of the environment; (2) the type of vegetation that influences the quality of the organic material and its degradability; and (3) the nature of the decomposition community, micro-organisms and soil fauna (Perin et al., 2010Perin A, Santos RHS, Caballero SSU, Guerra JGM & Gusmão LA (2010) Acúmulo e liberação de P, K, Ca e Mg em crotalária e milheto solteiros e consorciados. Revista Ceres, 57:274-281.). In similar climate and managements conditions, the variables that control the process of decomposition are the soil decomposition community and chemical quality of plant residues added to the soil (Brito, 2003Brito EC (2003) Adubação verde e sua influência em alguns atributos microbiológicos e químicos de um argissolo vermelho-amarelo sob cultivo de maracujá. Master Dissertation. Universidade Estadual do Norte Fluminense Darcy Ribeiro, Campos dos Goytacazes. 116p.).

The use of green manure plants, mainly from the Fabaceae family, set in rotation, succession, or consortium with crops of economic interest, is a viable option in the maintenance or recovery of soil quality by providing nutrients (e.g., N) to subsequent cultures, which reduces dependence on mineral fertilizers in agroecosystems (O’Dea et al., 2015O’Dea JK, Jones CA, Zabinski CA, Miller PR & Keren IN (2015) Legume, cropping intensity, and N-fertilization effects on soil attributes and processes from an eight-year-old semiarid wheat system. Nutrient Cycling in Agroecosystems, 102:179-194.). This is attributed to the ability of these species to incorporate atmospheric N through biological nitrogen fixation (BNF), recycle and mobilize nutrients from subsurface soil layers to surface horizons, increase the soil organic matter content, and consequently favor the edaphic biological activity (Sharma & Behera, 2009Sharma AR & Behera UK (2009) Nitrogen contribution through Sesbania green manure and dual-purpose legumes in maize-wheat cropping system: agronomic and economic considerations. Plant Soil, 325:289-304.).

The qualitative characteristics of plant residues (e.g., contents of C, N, lignin, hemicellulose, and polyphenols) strongly influence the dynamics of decomposition and release of nutrients in the soil (Swift et al., 1979Swift MJ, Heal OW & Anderson JM (1979) Decomposition in terrestrial ecosystems. Berkeley, University of California Press. 372p.; Palm, 1995Palm CA (1995) Contribution of agroforestry trees to nutrient requirements in intercropped plants. Agroforestry Systemys, 30:105-124.; Mafongoya et al., 1998Mafongoya PL, Giller KE & Palm CA (1998) Decomposition and nitrogen release patterns of tree prunings and litter. Agroforestry Systems, 38:77-97.; Monteiro & Gama-Rodrigues, 2004Monteiro MT & Gama-Rodrigues EF (2004) Carbono, nitrogênio e atividade da biomassa microbiana em diferentes estruturas de serapilheira de uma floresta natural. Revista Brasileira de Ciências do Solo, 28:819-826.). Several studies have identified the influence of Fabaceae plant residue quality on decomposition rates and the release of nutrients in the soil (Palm & Sanchez, 1991Palm CA & Sanchez PA (1991) Nitrogen release from the leaves of some tropical legumes as affected by their lignin and polyphenolic contents. Soil Biology Biochemistry, 23:83-88.; Cobo et al., 2002aCobo JG, Barrios E, Kass DCL & Richard T (2002a) Nitrogen mineralization and crop uptake from surface-applied leaves of green manure species on a tropical volcanic-ash soil. Biology and Fertility of Soils, 36:87-92.; Cobo et al., 2002bCobo JG, Barrios E, Kass DCL & Thomas RJ (2002b) Decomposition and nutrient release by green manures in a tropical hillside agroecosystem. Plant and Soil, 240:331-342.; Gama-Rodrigues et al., 2007Gama-Rodrigues AC, Gama-Rodrigues EF & Brito EC (2007) Decomposição e Liberação de Nutrientes de Resíduos Culturais de Plantas de Cobertura em Argissolo Vermelho-Amarelo na Região Noroeste Fluminense (RJ). Revista Brasileira de Ciências do Solo, 31:1421-1428.; Mahama et al., 2016Mahama GY, Vara Prasad PV, Roozeboom KL, Nippert JB & Rice CW (2016) Cover Crops, Fertilizer Nitrogen Rates, and Economic Return of Grain Sorghum. Agronomy Journal, 108:01-16.; Pereira et al., 2016Pereira NS, Soares I & Miranda FR (2016) Decomposition and nutrient release of leguminous green manure species in the Jaguaribe-Apodi region, Ceará, Brazil. Ciência Rural, 46:970-975.; Veras et al. 2016Veras MS, Ramos MLG, Daiana Nara Santos, Oliveira CCF, Carvalho AM, Pulrolnik K & Souza KW (2016) Cover Crops and Nitrogen Fertilization Effects on Nitrogen Soil Fractions under Corn Cultivation in a No-Tillage System. Revista Brasileira de Ciências do Solo, 40:e0150092.). A study on cover crops with contrasting chemical characteristics showed that the pigeon pea (C. cajan) had higher lignin content (32%) in the period chosen for its pruning compared to other species (Carvalho et al., 2011Carvalho AM, Pereira LL, Alves PCAC, Junior Guimarães R & Vivaldi LJ (2011) Cover plants with potential use for crop-livestock integrated systems in the Cerrado region. Pesquisa Agropecuária Brasileira, 46:1200-1205.). Due to the high recalcitrance level of the lignin molecule (Swift et al., 1979Swift MJ, Heal OW & Anderson JM (1979) Decomposition in terrestrial ecosystems. Berkeley, University of California Press. 372p.), the largest content in pigeon pea explains the lower rate of decomposition of the plant shoot of this Fabaceae. Carvalho et al. (2010)Carvalho AM, Dantas RA, Coelho CM, Lima WM, Souza JPP, Fonseca OP & Junior Guimarães R (2010) Teores de hemiceluloses, celulose e lignina em plantas de cobertura com potencial para sistema plantio direto no cerrado. Brasília, Embrapa Cerrados. 15p. (Boletim de Pesquisa e Desenvolvimento, 290). demonstrated that cellulose content of sunn hemp (C. juncea) was higher compared to other Fabaceae species and similar to wheat (Triticum spp., Poaceae family). In the same study, the lignin in the shoots of pigeon pea (C. cajan) was 71% higher compared to Urochloa humidicola (Poaceae family). These results reflected in lower rates of decomposition for sunn hemp and pigeon pea compared to other Fabaceae species studied.

To evaluate decomposition rates and nutrient release, several trials have been conducted in the field with Fabaceae and other species that do not realize the biological nitrogen fixation (Espindola et al., 2006Espindola JAA, Guerra JGM, Almeida DL, Teixeira MG & Urquiaga S (2006) Decomposição e liberação de nutrientes acumulados em leguminosas herbáceas perenes consorciadas com bananeira. Revista Brasileira de Ciências do Solo, 30:321-328.; Pleguezuelo et al., 2009Pleguezuelo CRR, Zuazo VHD, Fernández JLM, Peinado FJM & Tarifa DF (2009) Litter decomposition and nitrogen release in a sloping Mediterranean subtropical agroecosystem on the coast of Granada (SE, Spain): Effects of floristic and topographic alteration on the slope. Agriculture, Ecosystems and Environment, 134:79-88.; Meyer et al, 2011Meyer WM, Ostertag R & Cowie RH (2011) Macro-invertebrates accelerate litter decomposition and nutrient release in a Hawaiian rainforest. Soil Biology & Biochemistry, 43:206-211.). The coefficient k expresses the weight loss kinetics of decomposing organic materials, and through this index, ecosystems in many regions were studied (Olson, 1963Olson JS (1963) Energy storage and the balance of producers and decomposers in ecological systems. Ecology, 44:322-331.; Forey et al., 2015Forey E, Trap J & Aubert M (2015) Liming impacts Fagus sylvatica leaf traits and litter decomposition 25 years after amendment. Forest Ecology and Management, 353:67-76.). In a study of the decomposition of plant species, k values vary with latitude, temperature, precipitation, concentration of nutrients, and the C/N ratio of the species (Zhang et al., 2008Zhang D, Hui D, Luo Y & Zhou G (2008) Rates of litter decomposition in terrestrial ecosystems: global patterns and controlling factors. Journal of Plant Ecology, 01:85-93.).

In addition to the amounts of biomass and nutrients accumulated by Fabaceae, it is of fundamental importance to know the dynamics by which these nutrients become available in order to identify the best management for the use of these green manure (Matos et al., 2011Matos ES, Cardoso IM, Souto RL, Lima PC & Mendonça ES (2011) Characteristics, residue decomposition, and carbon mineralization of leguminous and spontaneous plants in coffee systems. Communications in Soil Science and Plant Analysis, 42:489-502.). Therefore, it is imperative to know indices related to the decomposition processes and release of nutrients in different situations in order to determine, among other issues, the most appropriate time to deploy and manage these fertilizer species (Matos et al., 2008Matos ES, Mendonça ES, Lima PC, Coelho MS, Mateus RF & Cardoso IM (2008) Green manure in coffee systems in the region of Zona da Mata, Minas Gerais: characteristics and kinetics of carbon and nitrogen mineralization. Revista Brasileira de Ciências do Solo, 32:2027-2035.). This knowledge improves crops of economic interest like Robusta coffee (Coffea canephora), a crop of great economic and social importance to the state of Espirito Santo, Brazil (Fassio & Silva, 2007Fassio LH & Silva AES (2007) Importância econômica e social do café conilon. In: Ferrão RG, Fonseca AFA, Bragança SM, Ferrão MAG & De Muner LH (Eds.) Café conilon. Vitória, Incaper. p.37-52.). It is noteworthy that studies of this type with Fabaceae at conditions in this Brazilian state are unknown. The objective of this work was to study the dynamics of decomposition and release of accumulated macronutrients in species of tropical green manure.

MATERIALS AND METHODS

Area of study and treatments

The experiment was setup on a farm located in the city of Cachoeiro de Itapemirim, in the southern of the Espirito Santo state (latitude 20º 45’ 11” South and longitude 41º 17’ 39” West). The climate is Cwa, having rainy summers and dry winters according to the Köppen classification, with the highest rainfall occurring in March, November, and December (Figure 1).

Figure 1
Monthly rainfall and number of rainy days during 2010, Cachoeiro de Itapemirim, Espirito Santo.

The soil was classified as a Udox (Soil Survey Staff, 2010Soil Survey Staff (2010) Keys to Soil Taxonomy. 11º ed. Washington, USDANRCS. 346p.), and the physical and chemical characterization is detailed in Table 1.

Table 1
Physical and chemical characterization of the Oxisol at a depth of 0 to 20 cm

The experimental design was a randomized block design (RBD) in a 4x5 factorial using four species of green manure and five data collection times (0, 30, 60, 90 and 120 days), with three replications. The plant material used was the shoot of the jack bean (Canavalia ensiformis (L.) DC.), pigeon pea (Cajanus cajan var. flavus DC.), dwarf mucuna (Mucuna deeringiana (Bort) Merr.), and sunn hemp (Crotalaria juncea L.).

The samples of plant material were placed in individual decomposition bags (litterbags) in the form of green material. Each sample consisted of 30 g of Fabaceae plant shoot material proportional to the percentage of leaves/ flowers and stems/ branches of each species. The decomposition bags were made of polyethylene screen with 1.5 mm mesh openings and dimensions of 0.2 m x 0.2 m. The experiment was setup in February 2010, with the decomposition bags distribution on the soil surface of a Coffea canephora plantation.

Laboratory evaluations

Samples of the four species of Fabaceae collected on the day of experiment setup (time zero) and bags in each collection time were dried in an oven at 65 °C to constant weight. Later, the samples were weighed to determine the dry matter and ground to determine the contents of K (flame photometry), P (spectrophotometry with blue-molybdenum), and Ca and Mg (atomic absorption spectrophotometry) (Silva, 2009Silva FC (2009) Manual de análises químicas de solos, plantas e fertilizantes. 2ª ed. Brasília, Embrapa Informação Tecnológica. 627p.). The contents of C and N were determined by dry combustion in an elemental analyzer.

Data analyses

To evaluate the decomposition and nutrient release of Fabaceae after analysis of variance (ANOVA), contrasts were established for the absolute values of the remaining biomass (dry matter), residual levels of macronutrients, and C/N and C/P; the results were grouped according to Alvarez & Alvarez (2006)Alvarez VVH & Alvarez GAM (2006) Comparação de médias ou teste de hipótese? Contrastes! Viçosa, Sociedade Brasileira de Ciência do Solo. 10p. (Boletim Informativo SBCS, 31).. The first contrast (C1) was between jack bean, pigeon pea, and dwarf mucuna against sunn hemp. This contrast was established to verify differences between sunn hemp, the species with the largest remaining dry mass (DM) and C/N and C/P ratios, and others Fabaceae. The second contrast (C2) was established between the dwarf mucuna against the others three Fabaceae. The third contrast (C3) compared the less fibrous herbaceous species, jack bean and dwarf mucuna, against the more fibrous Fabaceae, sunn hemp and pigeon pea. The significance of contrasts was evaluated by an F test (P < 0.01 to P < 0.10), with the aid of SAEG software (Universidade Federal de Viçosa, 2005).

The study of the dynamics of decomposition and release of nutrients was followed by the simple exponential model (Rezende et al., 1999Rezende CP, Cantarutti RB, Braga J M, Gomide JÁ, Pereira JM, Ferreira E, Tarré R, Macedo R, Alves BJR, Urquiaga S, Cadisch G, Giller KE & Boddey RM (1999) Litter deposition and disappearance in Brachiaria pastures in the Atlantic forest region of the South of Bahia, Brazil. Nutrient Cycling Agroecosystems, 54:99-112.): X = X0 ekt, where X is the amount of dry matter or nutrient remaining after a period of time t in days; X0 is the amount of dry matter or initial nutrient content; and k is the decay constant, which can be obtained by the equation: k = –ln(X/X0)/t. The coefficients of the regression models were tested using the t test at 1 and 5%.

The half-life (t1/2) was also estimated as it expresses the time required for half of the residue to decompose or for half of the nutrients contained in such residue to be released. It is possible to calculate the half-life time by the equation: t1/2 = ln (2)/k, where: t1/2 is the half-life of the dry material or nutrients; ln (2) is a constant value; and k is the constant of decomposition described above (Rezende et al., 1999Rezende CP, Cantarutti RB, Braga J M, Gomide JÁ, Pereira JM, Ferreira E, Tarré R, Macedo R, Alves BJR, Urquiaga S, Cadisch G, Giller KE & Boddey RM (1999) Litter deposition and disappearance in Brachiaria pastures in the Atlantic forest region of the South of Bahia, Brazil. Nutrient Cycling Agroecosystems, 54:99-112.). The decomposition constant k was subjected to ANOVA F test, and when significant, we used the t test at 5% probability according Thönnissen et al. (2000)Thönnissen C, Midmore DJ, Ladha JK, Olk DC & Schmidhalter U (2000) Legume decomposition and nitrogen release when applied as green manures to tropical vegetable production systems. Agronomy Journal, 92:253-260.. The statistical analysis was performed with the aid of SAEG software (Universidade Federal de Viçosa, 2005Universidade Federal de Viçosa (2005) SAEG: Sistema para análise estatística. Versão 9.0. Viçosa, Fundação Arthur Bernardes – Funarbe. CD-ROM.).

RESULTS

Chemical characteristics of Fabaceae residues

The initial N content in the plant species residues ranged from 19.1 to 40.7 g kg-1, being lower for sunn hemp and higher for dwarf mucuna (Table 2). For K, the range was 6.9 to 12.8 g kg-1, with sunn hemp having the lowest value and jack bean as the highest. As for the P, the variation was 3.3 to 5.4 g kg-1.

The C/N ratio ranged from 9.9 to 21.3, dwarf mucuna having the lowest value and sunn hemp having the largest (Table 2). For the C/P ratio, the dwarf mucuna had the lowest value (76), while pigeon pea and jack bean obtained the highest ratios, with 121 and 122, respectively.

Decomposition of green manure residues

The production of dry matter (DM) of shoots ranged from 3.9 to 12.5 Mg ha-1, being lower for dwarf mucuna and greater for sunn hemp (Mangaravite et al., 2014Mangaravite JCS, Passos RR, Andrade FV, Burak DL & Mendonça ES (2014) Phytomass production and nutrient accumulation by green manure species. Revista Ceres, 61:732-739.). The DM decomposition kinetics of these residues showed a similar behavior between the four species with exponential decay over time (Figure 2).

Table 2
Chemical characteristics of the tropical Fabaceae used in the study
Figure 2
Decomposition of the biomass of the four green manure plants, in the period 120 days, in percentage data. Jack bean (Canavalia ensiformis), pigeon pea (Cajanus cajan), dwarf mucuna (Mucuna deeringiana) and sunn hemp (Crotalaria juncea).

The same pattern of biomass decomposition was observed between the two more fibrous species, pigeon pea and sunn hemp, and the two less fibrous species, jack bean and dwarf mucuna. The less fibrous Fabaceae showed loss of dry matter (DM) mass of over 40% in the first 30 days of the experiment, while the more fibrous species lost only 20% in this period. It should be noted, therefore, that pigeon pea and sunn hemp species had larger amounts of DM over the whole period of decomposition.

The constant of decomposition k increased in the following order: sunn hemp < pigeon pea < dwarf mucuna < jack bean, which resulted in differences for the half-life time (t1/2) being 130.8, 99.0, 70.7, and 60.8 days, respectively (Table 3).

Table 3
Estimation of the parameters (X0, k) of the decomposition and nutrient release equation and the half-life (t1/2) for the green manure species

In contrast C2, it is evident that the dwarf mucuna shoot residue showed more effective decomposition of DM compared to others Fabaceae (Table 4). Moreover, contrast C1 demonstrates that the sunn hemp species had a lower DM decomposition rate.

Nutrient release

The less fibrous Fabaceae, jack bean and dwarf mucuna, compared with sunn hemp and pigeon pea, demonstrated higher rates of release of N, C, K and Mg in contrast C3 (Table 4). The remaining values for P did not appear as different between the more fibrous and less fibrous species (C3 contrast).

Table 4
Values and significance by the F test for the contrasts C1, C2 and C3, established between means of the variables DM, N, P, K, C, Ca, Mg, C/N and C/P, relative to remaining residuals of the decomposition of shoot of the Fabaceae species used as green manure

The release curves for K showed uniform pattern and were similar between the four Fabaceae (Figure 3). Regardless of species, 80% of K was released within the first 30 days of plant material exposure, which demonstrates the high initial rate of release of this element.

Figure 3
Evolution of the release of C, N, K and P, from the biomass of four green manure plants, over 120 days. Jack bean (Canavalia ensiformis), pigeon pea (Cajanus cajan), dwarf mucuna (Mucuna deeringiana) and sunn hemp (Crotalaria juncea).

The k mineralization constant for the K ranged from 0.0190 to 0.0273 g g-1dia-1 for sunn hemp and jack bean, respectively. This behavior was reflected in higher and lower t1/2 of K for sunn hemp and jack bean as values of 36.5 and 25.4 days, respectively (Table 3).

The four Fabaceae followed a similar P release pattern, especially from 90 days (Figure 3). These results are supported by the nearly k mineralization values ranging from 0.0201 to 0.0238 g g-1dia-1 and the half-lives (t1/2), which ranged from 34.5 to 29.1 days for the jack bean and sunn hemp, respectively (Table 3).

For N, the jack bean species had the highest release coefficient (k = 0.0122 g g-1 dia-1) associated with the lowest t1/2 value of 56.8 days (Table 3 and Figure 3). This indicates that release of 50% of N from this species occurred until the beginning of April 2010. After 120 days, in mid-June, the remaining N in this species was 18.4% (i.e., 81.6% of N was mineralized).

Among the studied nutrients, Ca showed the lowest rate of release between jack bean, dwarf mucuna, and pigeon pea, as evidenced by reduced k values and high half-life values (t1/2) (Table 3).

The Mg release pattern of the four Fabaceae had a behavior similar to N and K, with the highest release in the first 30 days (Figure 4). However, the t1/2 values for Mg are greater than those observed for K (Table 3). The t1/2 Mg values of the two most herbaceous Fabaceae, jack bean and dwarf mucuna were similar, while the same occurred with the two shrub species, pigeon pea and sunn hemp, with 84.5 values and 82 5 days, respectively (Table 3).

Figure 4
Evolution of the release of Ca and Mg from the biomass of four legumes with green manure, over 120 days. Jack bean (Canavalia ensiformis), pigeon pea (Cajanus cajan), dwarf mucuna (Mucuna deeringiana) and sunn hemp (Crotalaria juncea). *, ** = significant at 5% and 1% probability, respectively, by the t test.

DISCUSSION

Chemical characteristics of Fabaceae residues

Organic residues with concentrations greater than 20 g kg-1 and 2.5 g kg-1 for N and P, respectively, can be considered high quality (Mafongoya et al., 1998Mafongoya PL, Giller KE & Palm CA (1998) Decomposition and nitrogen release patterns of tree prunings and litter. Agroforestry Systems, 38:77-97.); however, for example, lignin and polyphenols can control the availability of these nutrients (Gentile et al., 2008Gentile R, Vanlauwe B, Chivenge P & Six J (2008) Interactive effects from combining fertilizer and organic residue inputs on nitrogen transformations. Soil Biology & Biochemistry, 40:2375-2384.). Taking the N and P contents into account, except for the sunn hemp N, the Fabaceae of our study are within the limit and, therefore, considered high quality.

Organic residues with initial C/N ratios < 20 and C/P ratios < 200 are considered high quality, being the predominant mineralization process to increase the availability of nutrients (Stevenson, 1986Stevenson FJ (1986) Cycles of soil: carbon, nitrogen, phosphorus, sulfur, micronutrientes. New York, John Wiley. 380p.). For C/P ratios, all of the Fabaceae fit in the category of high quality as suggested by Stevenson (1986)Stevenson FJ (1986) Cycles of soil: carbon, nitrogen, phosphorus, sulfur, micronutrientes. New York, John Wiley. 380p., and only the sunn hemp C/N ratio did not fit in high quality threshold.

Decomposition of green manure residues

The climate has a strong influence on the decomposition rates of plant residues between geographic regions; however, the chemical composition of the residue (e.g., C, N, cellulose, hemicellulose, polyphenols and lignin) is the best descriptor of decomposition locally (Adl, 2003Adl SM (2003) The ecology of soil decomposition. Wallingford, CABI. 335p.). In this sense, the C/N and C/P are important variables that locally influence the decomposition of plant residues added to the soil (Moreira & Siqueira, 2006Moreira FMS & Siqueira JO (2006) Microbiologia e bioquímica do solo. 2ª ed. Lavras, Editora UFLA. 729p.). In our study, the biomass of sunn hemp and pigeon pea had higher initial C/N relations compared to others Fabaceae, which may have contributed to the greater accumulation of their biomasses throughout the experimental period.

The chemical composition of plant species used in our study are well described and ratified in the literature (Gama-Rodrigues et al., 2007Gama-Rodrigues AC, Gama-Rodrigues EF & Brito EC (2007) Decomposição e Liberação de Nutrientes de Resíduos Culturais de Plantas de Cobertura em Argissolo Vermelho-Amarelo na Região Noroeste Fluminense (RJ). Revista Brasileira de Ciências do Solo, 31:1421-1428.; Carvalho et al. 2011Carvalho AM, Pereira LL, Alves PCAC, Junior Guimarães R & Vivaldi LJ (2011) Cover plants with potential use for crop-livestock integrated systems in the Cerrado region. Pesquisa Agropecuária Brasileira, 46:1200-1205.; Veras et al., 2016Veras MS, Ramos MLG, Daiana Nara Santos, Oliveira CCF, Carvalho AM, Pulrolnik K & Souza KW (2016) Cover Crops and Nitrogen Fertilization Effects on Nitrogen Soil Fractions under Corn Cultivation in a No-Tillage System. Revista Brasileira de Ciências do Solo, 40:e0150092.). For the same period evaluated, for example, the levels of lignin, cellulose and polyphenols were higher in shoot residues of sunn hemp and pigeon pea compared to jack bean and the dwarf mucuna. This causes sunn hemp and pigeon pea residues to have slower decomposition, making it able to form a stable mulch able to protect the soil against erosion, besides of contribute to the increase of soil organic matter.

The decomposition rates of organic residues in tropical soils are higher compared to temperate regions (Adl, 2003Adl SM (2003) The ecology of soil decomposition. Wallingford, CABI. 335p.). In our study, we observed higher rates of decomposition for dwarf mucuna and jack bean. Therefore, we can infer that the sunn hemp and pigeon pea residues have great potential for use as mulch in tropical soils due to the lower rates of decomposition and greater accumulation in the soil over time.

Release of nutrients

The behavior observed for the decomposition rates of dry biomass reflected the release rates of C, N, K, and Mg. The release rates of these elements were higher, in general, for the jack bean and dwarf mucuna compared with sunn hemp and pigeon pea. Plant residues with lower C/N ratios that are associated with lower levels of recalcitrant organic molecules (e.g., lignin) and have higher nutrient mineralization rates (Swift et al., 1979Swift MJ, Heal OW & Anderson JM (1979) Decomposition in terrestrial ecosystems. Berkeley, University of California Press. 372p.; Monteiro & Gama-Rodrigues, 2004Monteiro MT & Gama-Rodrigues EF (2004) Carbono, nitrogênio e atividade da biomassa microbiana em diferentes estruturas de serapilheira de uma floresta natural. Revista Brasileira de Ciências do Solo, 28:819-826.) can provide large quantities of nutrients for subsequent crops (Espindola et al., 2005Espindola JAA, Guerra JGM & Almeida DL (2005) Uso de Leguminosas Herbáceas para Adubação Verde. In: Aquino AM & Assis RL (Eds.) Agroecologia: princípios e técnicas para uma agricultura orgânica sustentável. Brasília, Embrapa Informação Tecnológica. p.435-451.). In the tropical conditions of this study, you should choose to use jack bean or dwarf mucuna residues rather sunn hemp or pigeon pea residues if the intention is the supply of nutrients (e.g., subsequent crops) in smaller periods time.

High K release values from biomass in various cover crops (Fabaceae) was also observed in other studies conducted in various soil and climatic conditions (Giacomini et al., 2003Giacomini SJ, Aita C, Übner AP, Lunkes A, Guidini E & Mara EB (2003) Liberação de fósforo e potássio durante a decomposição de resíduos culturais em plantio direto. Pesquisa Agropecuária Brasileira, 38:1097-1104.; Espindola et al., 2006Espindola JAA, Guerra JGM, Almeida DL, Teixeira MG & Urquiaga S (2006) Decomposição e liberação de nutrientes acumulados em leguminosas herbáceas perenes consorciadas com bananeira. Revista Brasileira de Ciências do Solo, 30:321-328.; Gama-Rodrigues et al., 2007Gama-Rodrigues AC, Gama-Rodrigues EF & Brito EC (2007) Decomposição e Liberação de Nutrientes de Resíduos Culturais de Plantas de Cobertura em Argissolo Vermelho-Amarelo na Região Noroeste Fluminense (RJ). Revista Brasileira de Ciências do Solo, 31:1421-1428.; Pereira et al., 2016Pereira NS, Soares I & Miranda FR (2016) Decomposition and nutrient release of leguminous green manure species in the Jaguaribe-Apodi region, Ceará, Brazil. Ciência Rural, 46:970-975.). K is the most abundant ion in plant cells (Marschner, 1997Marschner H (1997) Mineral nutrition of higher plants. 2º ed. London, Academic Press. 889p.), and its high speed of release can be attributed to the fact that it is present in ionic form, not being attached to any structural component of plant tissue (Gama-Rodrigues & Barros, 2002Gama-Rodrigues AC & Barros NF (2002) Ciclagem de nutrientes em floresta natural e em plantios de eucalipto e de dandá no sudeste da Bahia, Brasil. Revista Árvore, 26:193-207.; Costa et al., 2005Costa GS, Gama-Rodrigues AC & Cunha GM (2005) Decomposição e liberação de nutrientes da serapilheira foliar em povoamentos de Eucalyptus grandis no norte fluminense. Revista Árvore, 29:563-570.; Gama-Rodrigues et al., 2007Gama-Rodrigues AC, Gama-Rodrigues EF & Brito EC (2007) Decomposição e Liberação de Nutrientes de Resíduos Culturais de Plantas de Cobertura em Argissolo Vermelho-Amarelo na Região Noroeste Fluminense (RJ). Revista Brasileira de Ciências do Solo, 31:1421-1428.; Taiz & Zeiger, 2009Taiz L & Zeiger E (2009) Fisiologia Vegetal. 4ª ed. Porto Alegre, Artmed. 848p.). This rapid release of K to the soil suggests that the period of implementation of agricultural crops in succession to green manure should be reduced in order to reduce losses of K, seeking their greater use by subsequent crops. Furthermore, similar t1/2 values for K and P in the four studied Fabaceae species may facilitate the synchronization of agricultural management for the supply of these nutrients for agricultural crops in succession.

Fabaceae residues, unless they contain high levels of lignin and polyphenols, easily release N from the biomass (Palm & Sanchez, 1991Palm CA & Sanchez PA (1991) Nitrogen release from the leaves of some tropical legumes as affected by their lignin and polyphenolic contents. Soil Biology Biochemistry, 23:83-88.; Constantinides & Fownes, 1994Constantinides M & Fownes JH (1994) Nitrogen mineralization from leaves and litter of tropical plants: relationship to nitrogen, lignin and soluble polyphenol concentrations. Soil Biology and Biochemistry, 26:49-55.; Palm, 1995Palm CA (1995) Contribution of agroforestry trees to nutrient requirements in intercropped plants. Agroforestry Systemys, 30:105-124.; Cobo et al., 2002aCobo JG, Barrios E, Kass DCL & Richard T (2002a) Nitrogen mineralization and crop uptake from surface-applied leaves of green manure species on a tropical volcanic-ash soil. Biology and Fertility of Soils, 36:87-92.). A study conducted in tropical soil evaluating the decomposition and release of nutrients from Fabaceae and non-Fabaceae species residues found that the N release rate was higher for the jack beans compared to the other species tested. The values for the coefficient k and t1/2 were similar to our study with 0.0162 g g-1 dia-1 and 43 days, respectively (Gama-Rodrigues et al., 2007Gama-Rodrigues AC, Gama-Rodrigues EF & Brito EC (2007) Decomposição e Liberação de Nutrientes de Resíduos Culturais de Plantas de Cobertura em Argissolo Vermelho-Amarelo na Região Noroeste Fluminense (RJ). Revista Brasileira de Ciências do Solo, 31:1421-1428.). These authors related these results to better chemical quality of the jack bean residue, due to higher levels of N, P, and Ca, as well as lower ratios of C/N and polyphenol/N.

The N released from jack bean until the half-life (t1/2) and 120 days after the onset of decomposition corresponded to 102.4 and 167.1 kg ha-1, respectively. For an expected yield of Coffea canephora fruits between 31-50 sacks ha-1, it is recommended to perform nitrogen fertilization of 320 kg ha-1 N (Prezotti et al., 2007Prezotti LC, Bragança SM, Martins AG & Lani JÁ (2007) Calagem e adubação. In: Ferrão RG, Fonseca AFA, Bragança SM, Ferrão MAG & De Muner LH (Eds.) Café conilon. Vitória, Incaper. p.341-342.). Thus, if the goal is synchronizing the partial supply of N for C. canephora from jack bean decomposition, it can be inferred that the values of N released by jack bean in t1/2 and 120 days are, respectively, between 32 and 52% of the total N required to achieve that average yield of coffee.

The low release rate behavior of Ca of plant biomass is often reported in the literature for Fabaceae species and other non-Fabaceae (Cobo et al., 2002bCobo JG, Barrios E, Kass DCL & Thomas RJ (2002b) Decomposition and nutrient release by green manures in a tropical hillside agroecosystem. Plant and Soil, 240:331-342.; Espindola et al., 2006Espindola JAA, Guerra JGM, Almeida DL, Teixeira MG & Urquiaga S (2006) Decomposição e liberação de nutrientes acumulados em leguminosas herbáceas perenes consorciadas com bananeira. Revista Brasileira de Ciências do Solo, 30:321-328.; Gama-Rodrigues et al., 2007Gama-Rodrigues AC, Gama-Rodrigues EF & Brito EC (2007) Decomposição e Liberação de Nutrientes de Resíduos Culturais de Plantas de Cobertura em Argissolo Vermelho-Amarelo na Região Noroeste Fluminense (RJ). Revista Brasileira de Ciências do Solo, 31:1421-1428.; Perin et al., 2010Perin A, Santos RHS, Caballero SSU, Guerra JGM & Gusmão LA (2010) Acúmulo e liberação de P, K, Ca e Mg em crotalária e milheto solteiros e consorciados. Revista Ceres, 57:274-281.). This behavior is associated with the fact that this nutrient is one of the middle lamella of the cell wall constituents and one of the most recalcitrant components of plant tissues (Taiz & Zeiger, 2009Taiz L & Zeiger E (2009) Fisiologia Vegetal. 4ª ed. Porto Alegre, Artmed. 848p.; Perin et al., 2010Perin A, Santos RHS, Caballero SSU, Guerra JGM & Gusmão LA (2010) Acúmulo e liberação de P, K, Ca e Mg em crotalária e milheto solteiros e consorciados. Revista Ceres, 57:274-281.).

The similarity of Mg and K in terms of the release dynamics during the first 30 days may be associated to the fact that Mg is also in ionic form within the plant tissue (Waters, 2011Waters BM (2011) Moving magnesium in plant cells. New Phytologist, 190:510-513.). It is noteworthy that over 70% of Mg diffuses freely in the cell suspension or is bound by ionic bonds to negatively charged components (e.g., proteins) (Dechen & Nachtigall, 2007Dechen AR & Nachtigall GR (2007) Elementos requeridos à nutrição de plantas. In: Novais RF, Alvarez VVH, Barros NF, Fontes RLF, Cantarutti RB & Neves JCL (Eds.) Fertilidade do Solo. Viçosa, Sociedade Brasileira de Ciência do Solo. p.91-132.). The N is part of proteins and together with Mg is a structural component of chlorophyll (Cantarella, 2007Cantarella H (2007) Nitrogênio. In: Novais RF, Alvarez VVH, Barros NF, Fontes RLF, Cantarutti RB & Neves JCL (Eds.) Fertilidade do Solo. Viçosa, Sociedade Brasileira de Ciência do Solo. p.375-470.; Waters, 2011Waters BM (2011) Moving magnesium in plant cells. New Phytologist, 190:510-513.); this may be one of the explanations for similar behavior in the dynamic mineralization between Mg and N.

CONCLUSIONS

Among the species tested, sunn hemp showed the lowest rate of decomposition, next to the pigeon pea, inferring that shrub species have higher potential to accumulate organic matter and act as mulch in tropical edaphoclimatic conditions. On the other hand, jack beans and dwarf mucuna should be chosen if the objective is the supply of nutrients in shorter periods for subsequent crops because they demonstrated higher rates of decomposition and nutrient release during experiment.

The K and P for the four Fabaceae showed similar t1/2 values, and for N, sunn hemp was the species that presented the lowest coefficient of mineralization (k = 0.0040 g g-1 dia-1), associated with greater t1/2 (173.3 days). On the other hand, jack bean was the species that showed the highest coefficient of mineralization for N (k = 0.0122 g g-1 dia-1), associated with the lower half-life (t1/2 = 56.8 days).

ACKNOWLEDGEMENTS, FINANCIAL SUPPORT AND FULL DISCLOSURE

The authors would like to thank Incaper (Capixaba Institute of Research, Technical Assistance and Rural Extension) for the logistical support as well as FAPES (Espirito Santo Research and Innovation Support Foundation) and CNPq (Brazilian National Research Council) for financial support.

There is no conflict of interests in carrying the research and publishing the manuscript.

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Publication Dates

  • Publication in this collection
    16 June 2023
  • Date of issue
    May-Jun 2023

History

  • Received
    05 Aug 2020
  • Accepted
    19 Sept 2022
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