Cover crops on soil quality and yield of cowpea under no-tillage in the Amazon savanna

. Conservation practices such as no-tillage are necessary to maintain, and/or improve agricultural soil quality. However, straw formation and maintenance in tropical regions is a limiting factor to adopting this system. In this sense, this research aimed to study the effect of cover crops on straw formation, soil quality indicators, and cowpea yield under no-tillage in the Amazon savanna. Two experiments were carried out in consecutive years, on a Latossolo Amarelo . The treatments consisted of the straw of cover crops in a single ( S ) and intercrop ( I ) system, as follows: Urochloa brizantha (UB S ), Pennisetum glaucum (PG S ), Crotalaria juncea (CJ S ), Canavalia ensiformis (CE S ), Mucuna aterrima (MA S ), U. brizantha and C. juncea (UBCJ I ), U. brizantha and C. ensiformis (UBCE I ), P. glaucum and C. juncea (PGCJ I ), P. glaucum and C. ensiformis (PGCE I ), and spontaneous vegetation (SV). Cowpea was cultivated after desiccation of the cover crops. Most of the straw favored soil particle aggregation, except for C. juncea and SV, which negatively influenced this variable. Basal soil respiration, organic carbon content, potassium, base saturation, geometric mean diameter, macroaggregates, and macroporosity at layer of 0-0.10 m were the most sensitive indicators for improving soil quality in a savanna environment. UB S , UBCJ I , and UBCE I were superior to the other treatments in improving soil quality. Almost all treatments increased cowpea yield by up to 29%, except for CJ S and SV.


Introduction
Soil quality is defined by the set of attributes that respond to soil changes as a function of agronomic management practices, which can be evaluated indirectly through the selection and evaluation of indicators sensitive to soil changes (Zornoza et al., 2015;Panico, Memoli, Esposito, Maisto, & Marco, 2018).
These indicators are important to analyze the potential of conservationist management, such as the notillage system, which advocates the maintenance of soil cover, crop rotation, and minimum soil disturbance.The success of this system is related to the selection of cover species adapted to each type of soil and climate.Therefore, it is necessary to study and adapt the system in each region, especially where the climate (high temperatures and humidity) makes it difficult to form and maintain straw (Teixeira et al., 2018).
Thus, the use of species that produce more than 6 t ha −1 of dry mass on the soil per year (Nunes et al., 2006) and are capable of recycling nutrients is essential (Bertolini et al., 2019).Among plant species with this potential, the following stand out: Canavalia ensiformis and Mucuna aterrima (Fabaceae); Pennisetum glaucum and Urochloa spp.(Poaceae) (Pereira et al., 2017;Simon et al., 2019).
Poaceae species are important to maintain the balance of the carbon/nitrogen ratio (C/N) at adequate levels for straw maintenance on the soil.In contrast, Fabaceae species provide higher amounts of nitrogen (N) to the soil.However, the release of nutrients from crop residues must occur in sync with crop demand for maximum N use (Stute & Posner, 1995).In this sense, intercropping between these families can improve the use of beneficial characteristics and minimize the undesirable ones (Bertolini et al., 2019).
Acta Scientiarum.Agronomy, v. 46, e62853, 2024 Regarding to the no-tillage system, crop rotation practice allows the best use of soil nutrients since the plants have higher root dynamics in soil profile (Singh et al., 2018).In this practice, the use of species with higher economic returns to the farmer is essential, such as corn (Zea mays L.) (Stein & Steinmann, 2018), cowpea (Vigna unguiculata (L.) Walp), and common bean (Phaseolus vulgaris L.), crops that make up the basic diet of the population and have been gaining ground in this system in tropical countries.
In this context, human activities alter soil properties.Therefore, the most effective indicators for monitoring soil quality need to be clarified under the Amazon savanna conditions to make soil use viable, aiming at its conservation, preservation of its resilience, and the increase of crop yield without compromising its sustainability.In this context, this research aimed to study the effect of cover crops on straw formation, soil quality indicators, and cowpea yield under no-tillage in the Amazon savanna.

Material and methods
The study was carried out in the experimental area of the Agricultural Sciences Center of the Federal University of Roraima, Boa Vista, Roraima State, Brazil, on a Latossolo Amarelo distrófico (Typic Hapludox, Soil Taxonomy) (Anjos & Schad, 2018).The regional climate, according to the Köppen classification, is Aw, a rainy tropical climate.Monthly data on rainfall, mean temperature, and relative air humidity for the city of Boa Vista, Roraima State, Brazil, during the experiment are shown in Figure 1 (INMET, 2020).
Lime requirement was determined based on the soil analysis results.The area was prepared conventionally (one plowing and two harrowing practices), with the incorporation of 1,200 kg ha −1 of dolomitic limestone with 90% total neutralizing power in the 0.20 m soil depth.After soil correction, the area was divided into fixed plots of 30 m 2 (5 × 6 m), where cover crops (Urochloa brizantha, Pennisetum glaucum, Crotalaria juncea, Canavalia ensiformis, Mucuna aterrima, U. brizantha and C. juncea, U. brizantha and C. ensiformis, P. glaucum and C. juncea, and P. glaucum and C. ensiformis) were grown or the spontaneous vegetation was maintained, representing 10 treatments.Fertilization was carried out in the planting row of the cover crops using 30, 60, and 50 kg ha −1 of nitrogen, P 2 O 5 , and K 2 O in the form of urea, single superphosphate, and potassium chloride, respectively.
Cover crops and spontaneous vegetation were desiccated with glyphosate at a dose of 1.4 kg ha −1 at 70 days, before cowpea (BRS Guariba) planting.Corn of the Bandeirante variety was grown at the end of the bean cycle.The recommendation for crop fertilization was based on Uchôa et al. (2009) for cowpea and Ribeiro, Guimarães, and Alvarez (1999) for corn.The area was left fallow after this initial sequence of crop rotation and the first no-tillage crop was started in 2015.

Experiment and statistical design
Two experiments were conducted and evaluated between 2015 and 2017 in consecutive cycles, following the principles of the no-tillage system.Crop rotation involved the cover crops, cowpea (main crop), and corn.The agronomic evaluations were not performed in the corn crop, as it was cultivated to rotate with the predecessor species.
During the experiment, complementary irrigation was used by means of conventional sprinkler irrigation, using Fabrimar ECO A320 sprinklers, with a water depth of approximately 8 mm per day, whenever necessary.
Cover crop sowing (first cycle: April/2015 and second cycle: September/2016) was carried out manually in the experimental units at 70 days (Urochloa brizantha, Mucuna aterrima, and Canavalia ensiformis) and 55 days (Pennisetum glaucum and Crotalaria juncea) before cowpea planting.The desiccation of cover crops and spontaneous vegetation was performed using glyphosate (N-[phosphonomethyl]-glycine) at a dose of 1.4 kg ha −1 , applied using a knapsack sprayer.
At the time of desiccation, Urochloa brizantha and Mucuna aterrima were at the vegetative stage, Pennisetum glaucum at grain filling, and Crotalaria juncea and Canavalia ensiformis at full flowering.After desiccation, biomass samples of the treatments were collected from each experimental unit using a 0.25-m 2 hollow frame.The plant material contained in the area of the frame was oven-dried at 65°C for 72h to obtain the straw dry mass, expressed in kg ha −1 .
Cowpea (BRS Guariba) was sown 10 days after desiccation of the cover crops at an inter-row spacing of 0.5 m and ten seeds per linear meter.Subsequently, thinning was carried out and six plants remained per meter.Dry cowpea pods were manually harvested at 60 days after emergence (DAE) and packed in paper bags until they were manually threshed.The grains were weighed (g) and the moisture was measured (%) using a precision balance (0.01 g) and a moisture and impurity analyzer model G650, respectively.The values were transformed into kg ha −1 (yield estimate with moisture corrected to 13%).
Then, corn AG 1051 was sown at an inter-row spacing of 0.5 m and 3 plants per linear meter.This rotation sequence was repeated during the two cultivation cycles.The fertilization of cover crops, cowpea, and corn followed the initial fertilization.

Soil sampling
Soil samples were collected in the morning at a layer of 0-0.10 m from each experimental unit at full flowering of the cowpea crop (first and second cycles) for the evaluation of biological and chemical indicators.Four simple soil samples were collected in the inter-rows using an auger, at 10 cm away from the stem of the cowpea plants, to form a composite sample.
Disturbed and undisturbed soil samples were collected from the center of each experimental unit at 0-0.15 and 0.15-0.30m layers at the end of the cowpea cultivation (only in the second cycle).The disturbed samples were collected in the inter-rows of the cowpea crop using a hoe, while the undisturbed samples were collected using 100-cm 3 volumetric rings.The material was transported to the laboratory and analyses were performed.

Biological indicators of soil quality
Part of the undisturbed soil samples was kept in the shade, during the collection phase, inside a styrofoam box.Then, these samples were passed through a 2-mm mesh sieve in the laboratory at 24°C, packed in plastic bags, and stored in a refrigerator (4°C).The following variables were evaluated: basal soil respiration (BSR) by the method proposed by Jenkinson and Powlson (1976) and microbial biomass carbon (MBC) according to the methodology of Vance, Brookes, and Jenkinson (1987).The metabolic quotient (qCO 2 ) was calculated using the values obtained from BSR and MBC by dividing the daily mean of the C-CO 2 evolved from the soil by the MBC determined in the soil.

Soil chemical properties
Part of the disturbed soil samples was air-dried and passed through 2-mm mesh sieves for further analysis of: pH (H 2 O); soil organic carbon (SOC); available phosphorus (P) and potassium (K + ); exchangeable calcium (Ca 2+ ), magnesium (Mg 2+ ), and aluminum (Al 3+ ); and potential acidity (H + Al), according to Teixeira, Donagemma, Fontana, and Teixeira (2017).The sum of bases (SB) and base saturation (V) were estimated based on these properties.

Statistical analysis
The data obtained in each year were subjected to individual analysis of variance by the F-test (p ≤ 0.05).The joint analysis of the data was carried out when the mean squared residual ratio was lower than 7:1.The means of the variables were grouped using the Scott-Knott test (p ≤ 0.05).The analyses were performed using the statistical program SISVAR version 5.6 (Ferreira, 2014).A multivariate principal components analysis was applied to determine the correlation between treatments and the analyzed variables using the Infostat statistical package (Di-Rienzo et al., 2008).

Results and discussion
Biological indicators of soil quality were affected by cover crops and crop cycles.BSR was higher in the soil cultivated with UB S , PG S , CE S , and PGCE I , regardless of the cycle, and higher in the first cycle, regardless of the cover crop (Table 1).This result may be related to climate factors (Figure 1) during the experimental time, as the first cycle presented an imbalance relative to qCO 2 although it promoted a higher BSR value.According to Cattelan and Vidor (1990), this variable can be influenced by factors such as humidity, temperature, and soil nutrient availability.UB S , CJs, and the intercrop systems UBCJ I , UBCE I , and PGCJ I were grouped with the highest means of MBC in the first cycle, while CE S , MA S , UBCE I , and PGCE I were the cover crops that most favored MBC in the second cycle (Table 1).Moreover, the second cycle promoted the highest MBC values, except for UB S , CJ S , and SV, which showed cultivation cycles similar to each other.This result may be related to the low increase in dry mass that these plants promoted between crop cycles (Table 5).On the other hand, the increase in MBC is related to soil organic carbon accumulation promoted in the second crop cycle (Table 2).According to Melo, Silva, Evald, and Rocha (2017), well-managed crops quantitatively improve the soil microbial community, which contributes to the highest SOM values.
MBC is a sensitive indicator for monitoring human influences related to the soil.Studies have indicated good responses of this attribute on a dystrophic Red Latosol with Pennisetum glaucum, Urochloa brizantha, Raphanus sativus L., Crambe abyssinica Hochst, and Mucuna aterrima (Simon et al., 2019;Duarte et al., 2014).
The highest qCO 2 values in the first cycle were observed for UB S , CJ S , PG S , UBCJ I , UBCE I , PGCJ I , and SV.In the second cycle, qCO 2 did not differ between cover crops (Table 1).According to Saviozzi, Bufalino, Levi-Minzi, and Riffald (2002), this variable is an indicator that estimates the biological activity and substrate quality through the efficiency of the microbial biomass in using the available carbon for biosynthesis.
No effect of cover crops on soil pH was observed.However, the crop cycles influenced soil acidification, with more acidic pH in the second cycle (Table 2).This result was already expected since the crops extract soil bases.It may also be associated with nitrogen fertilization carried out in both cultivation years and the release of exudates from the roots of cover crops, as reported by Maluf, Soares, Silva, Neves, and Oliveira Silva (2015), who identified a reduction in soil pH over time due to the decomposition of plant residues, especially in soil under the influence of Urochloa and Stylosanthes.
SOC (Table 2) showed no difference between cover crops in the first cycle.The straws of UB S and UBCE I stood out in the second cycle with the best results.An increase in carbon was observed in the second cycle for UB S , PG S , MA S , and UBCE I compared to the first cycle.Evald et al. (2021) observed SOC sensitivity on soil management and its impact on soil quality.
Phosphorus (P) concentration in the soil was affected by cover crops and crop cycles, being higher when the soil was cultivated under SV, followed by PG S , CE S , and PGCE I (Table 2).Moreover, the content of this element was higher in the second cycle, regardless of the cover crop.Spontaneous vegetation could not immobilize mineral P, transforming it into organic P. Therefore, it remained in the form of available P, unlike the other crops, which presented higher straw and immobilized more P.This fact becomes important, as it stimulates microbial activity by increasing phosphatase activity (Fialho et al., 2020).
Thus, UB S , CJ S , MA S , and the intercrops UBCJ I , UBCE I , and PGCJ I possibly extracted more P from the system, being retained by the straw for a longer time, thus showing low cycling and, consequently, low concentration in the soil.
An isolated effect of the analyzed factors was observed for potassium (K), in which the cover crops UB S , CJ S , and the intercrops UBCJ I and UBCE I were those that most contributed to the cycling of K to the soil (Table 2).The second cycle provided an increase in soil K contents.This result can be associated with the nutrient cycling performed by cover crops and the fertilization in the second cycle since K is a mobile element in the soil and is very susceptible to leaching.According to Freitas et al. (2019), the cultivation of cover crops is an important strategy to reduce K losses by leaching and erosion in the soil, as cover crops are efficient in extracting and cycling this nutrient to the soil.
Cover crops and crop cycles alone influenced the calcium (Ca) content in the soil (Table 2).Cover crops grown under simple cultivation and the spontaneous vegetation were grouped with the best results and the first cycle presented the best mean.The lower Ca content in the second cycle may have been caused by its immobilization in the soil microbial biomass, following the stoichiometric relationship between carbon and nutrients in the organic compost and the nutritional requirements of soil-decomposing microorganisms or the very need for extraction of this nutrient by the crop (Sinsabaugh et al., 2008).
As observed for Ca, magnesium (Mg) and the sum of bases (SB) also presented an isolated effect for cover crops and crop cycles.The cover crops that stood out positively for both variables were UB S , PG S , CJ S , and SV, with the first cycle being superior compared to the second crop cycle (Table 3).Aluminum (Al), potential acidity (H + Al), and base saturation showed an isolated effect for cover crops and crop cycles.These variables presented no difference between cover crops.However, the second cycle was superior to the previous cycle, except for base saturation (Table 3).
These results are similar to those obtained by Silva et al. (2017), who also observed a reduction in the contents of Ca, Mg, H + Al, SB, total CEC after two years of cultivation with cover crops in succession with the common bean 'Perola'.
Regarding soil physical properties, cover plants did not influence soil density (1.61 and 1.59 g dm −3 ), macroporosity (26.25 and 25.76%), and total porosity (40.83 and 41.76%) in the evaluated layers, respectively.However, an isolated effect was verified for microporosity, with values of 14.57 and 16.00% for the studied layers, respectively.Likewise, Pessotto et al. (2016) observed the effect of cover crops on the microporosity in the 0-5 cm layer.However, no effect of the same plants was observed on soil density, demonstrating the impossibility of differentiating the most effective species in improving this property in the short term.
Table 4 shows a higher proportion of larger aggregate classes in the first layer for cover crops effect within layer levels when the soil was cultivated with UB S , CJ S , CE S , MA S , and the intercrops UBCJ I and PGCJ I .In contrast, the second layer showed an improvement in this soil property in the cultivation of CE S , MA S , and the intercrops UBCJ I and PGCE I .An improvement in the geometric mean diameter was observed in the 0.15-0.30m layer compared to the other layer when the soil was cultivated with the intercrops UBCE I and PGCE I .This result may be related to the root system of the cover crops.UB S and PG S have the ability to form a more robust and voluminous root system and CE S has a taproot with a length longer than 20 cm, which may have favored the improvement of aggregates in the 0.15-0.30cm.However, according to the aggregate stability method in water, the maximum aggregate stability would correspond to the GMD value equal to 5 mm.Therefore, two cultivation cycles under the no-tillage system were not enough to improve soil aggregation.
On the other hand, the use of cover crops under no-tillage system promotes, over time, an increase in organic carbon, which is responsible for soil aggregation.However, the higher amount of plant material deposited on the soil benefits soil aggregation and, consequently, decreases soil erodibility (Torres, Pereira, Assis, & Souza, 2015).Singh et al. (2018) evaluated a crop rotation system after three years of cultivation and found a higher predominance of stable macroaggregates in water (>30%) at a layer of 0-0.15 m in plots with crop residues on the soil surface.
The highest percentages of macroaggregates (Table 4) in the most superficial soil layer were observed in the soil with straw of CJ S , CE S , MA S , and the intercrop UBCJ I .In contrast, CE S , MA S , and the intercrops UBCJ I , UBCE I , and PGCE I were the cover crops that contributed to the highest values of this variable in the 0.15-0.30m layer.Regarding soil layers, CJ S provided a higher percentage of this variable in the first layer, while UBCE I and PGCE I contributed positively to macroaggregation in the second layer.In general, the geometric mean diameter is closely related to the percentage of soil aggregates, mainly macroaggregates (aggregates higher than 0.250 mm).
Thus, conservationist practices, including the no-tillage system, are essential to increase soil aggregate stability, as this system allows the maintenance of crop residues on the soil surface.According to Singh et al. (2018), the persistence of plant material on the soil favors the formation of water-stable macroaggregates in the first soil layers.
The lowest percentages of microaggregates were attributed to the first layer of the soil cultivated with CJ S , CE S , MA S , and the intercrop UBCJ I , as observed for the variables previously discussed.On the contrary, the cultivation of CE S , MA S , and the intercrops UBCJ I , UBCE I , and PGCE I provided the lowest percentages of this variable in the second layer (Table 4).Regarding the effect of layers within the level of cover crops, the lowest percentage of this variable was obtained in the first layer when the soil was under the influence of CJ S .The second layer presented lower values when the soil was cultivated with the intercrops UBCE I and PGCE I .
No differences were observed in the percentage of simple particles between the straws within the same studied layer.However, the comparison between layers showed that CJ S and the intercrop PGCJ I had lower means in the first layer, whereas SV had a lower percentage of single particles in the second layer (Table 4).
Acta Scientiarum.Agronomy, v. 46, e62853, 2024 An isolated effect of cover crops and crop cycles was observed on the dry mass of cover crops and cowpea yield (Table 5).UB S , PG S , and intercropped crops produced the highest amounts of dry mass.Legumes cultivated in a simple system were grouped with an intermediate mean, ahead of SV.Regarding the crop cycles, the second cycle stood out due to its best mean.
The cultivation on the straw of CJ S and SV had a negative influence on crop yield.The other cover crops did not differ from each other and were grouped as a function of the highest means.Regarding crop cycles, the second cycle was superior to the previous cycle.This result may be related to the improvement of biological (MBC and qCO 2 ) and chemical attributes (SOC, P, and K), which provided the trend of soil restructuring and increase in the biomass production of cover crops.Some divergences were observed when comparing these values with other studies, such as the dry mass production of Canavalia ensiformis and Crotalaria juncea, which stood out in the conditions of northwestern Rio Grande do Sul (subtropical climate), producing means of 24.99 and 22.71 t ha −1 , respectively (Pereira et al., 2017).This variation of cover crops on the soil surface in different regions was expected because the no-tillage system requires adaptations depending on the region (Teixeira et al., 2018).However, according to Nunes et al. (2006), the cover crops, except for spontaneous vegetation, presented dry mass production above the ideal, which is around 6 t ha −1 .In this sense and considering the dry mass production of cover crops, the evaluated plants have the potential to be used as cover crops under the conditions of this study.
In general, although cowpea presented low yield on the straw of CJ S and SV compared to the other treatments, the reached yields were higher than the national (533 kg ha −1 ), the North Region (845 kg ha −1 ), and Roraima means (1,151 kg ha −1 ) (IBGE, 2021).
Principal component analysis showed that components 1 and 2 accounted for approximately 56% of the variability of the first crop cycle data (Figure 2).Thus, cowpea yield was strongly correlated with P content, pH, and qCO 2 , and the cover crops associated with these variables were PG S , SV, and the intercrops PGCJ I and PGCE I .
Cover crop dry mass was more influenced by UB S and the intercrops UBCE I and UBCJ I , which form a group together with V, BSR, SOC, K, MBC, and SB.Moreover, Figure 2 shows an isolated group composed of Al and H + Al, which were correlated with CE S and MA S .
The second cycle (Figure 3) showed a correlation between CY and CCDM, reference variables, adjacent to BSR, V, SOC, and K, which were closely influenced by UB S and the intercrops UBCJ I and UBCE I .MA S and the intercrop PGCJ I correlated with MBC.A positive correlation was observed between CE S and Al.Another group can be observed in the correlation between P and H + Al, being influenced by SV and the intercrop PGCE I .The pH, qCO 2 , and SB were positively correlated with each other and influenced by PG S .For soil physical attributes, the soil cultivated with CJ S influenced the correlation between MICROAG(B), DS(B), MICROP(B), CCDM and CY (Figure 4).When analyzing the data, it is noticed that the values of these variables are related to the reduction in the production of dry mass of Crotalaria juncea in the soil and the production of cowpea.The variables DMG(A), MACROAG(A), MACROP(A) and PT(A) were positively correlated being influenced by CE S , MA S and the intercrop UBCJ I .There is another group was formed by the correlation between DS(A), PS(A) and MICROAG(A), these variables being influenced by UB S , PG S and the intercrop PGCE I and UBCE I .The treatment formed by VE influenced the correlation between MICROP(A), MACROP(B), PT(B) and DMG(B).The amount of straw formed by cover crops in the first cropping cycle presented little influence on cowpea production, which was more influenced by soil chemical and biological properties, especially P and qCO2, respectively.It may be related to the time required for system stabilization.However, the second cycle showed a positive correlation between the amount of dry mass produced by cover crops and cowpea yield.
The greater capacity to transform mineral P into organic P of the weeds in the SV area may have favored the accumulation of P in this area.Moreover, this population had little influence on soil acidification.In general, soil acidification can occur in the presence of plants of the legume family, as they release H+ during biological nitrogen fixation (Marschner, 1995).
UBS showed advantages regarding potassium cycling.For this reason, it may have favored the activity of soil microorganisms, which was verified through the improvement of BSR and MBC.Moreover, an increase in the sum of bases was observed when the soil was cultivated with U. brizantha, demonstrating the strong participation of potassium in this exchange complex.
CJS did not improve soil physical attributes, especially aggregation in the second layer, although it had a positive influence on some soil chemical attributes.It also presented low biomass production and low cowpea yield.Crop yield is related to the balance between soil biological, chemical, and physical attributes.However, Nouri, Lee, Yin, Tyler, and Saxton (2019) conducted a long-term study and reported that the physical attribute is closely related to the water dynamics in the soil and, consequently, to the crop yield.
The results found in the present study provide technical-scientific support regarding the use of cover crops to improve soil quality and, consequently, increase cowpea yield under experimental conditions.

Conclusion
Urochloa brizantha and the intercrops U. brizantha and Crotalaria juncea, and U. brizantha and Canavalia ensiformis stand out positively in improving soil quality.Basal soil respiration, soil organic carbon, potassium, base saturation, geometric mean diameter, macroaggregates, and macroporosity in the 0-0.10 m layer are the most sensitive indicators for improving soil quality in a savanna environment.U. brizantha, Pennisetum glaucum, C. ensiformis, Mucuna aterrima, and intercrop systems increase cowpea yield by up to 29% relative to spontaneous vegetation.
the Institutional Research Support Program of Federal University of Roraima (PROPESQUISA/PRPPG-UFRR).

Table 1 .
Basal soil respiration (BSR), soil microbial biomass carbon (MBC), and soil metabolic quotient (qCO2) as a function of different cover crops and crop cycles on a Latossolo Amarelo of the Amazon savanna, Boa Vista, Roraima State, Brazil, 2017.
CC BSR

Table 2 .
Soil pH (H2O) and contents of organic carbon, phosphorus, potassium, calcium, and magnesium as a function of different cover crops and crop cycles on a Latossolo Amarelo of the Amazon savanna, Boa Vista, Roraima State, Brazil, 2017.

Table 3 .
Sum of base (SB), aluminum (Al), potential acidity (H + Al), and base saturation (V) as a function of different cover crops and crop cycles on a Latossolo Amarelo of the Amazon savanna, Boa Vista, Roraima State, Brazil, 2017.

Table 4 .
Geometric mean diameter, macroaggregates, microaggregates, and simple particles evaluated in two layers of a Latossolo Amarelo as a function of different cover crops and crop cycles in the Amazon savanna, Boa Vista, Roraima State, Brazil, 2017.Means followed by the same uppercase letter in the row and lowercase letter in the column belong to the same cluster by the Scott-Knott test at a 5% probability.m = mean; CC = cover crops; Canavalia ensiformis; MAS = Mucuna aterrima; I = intercrop system; UBCJI = U. brizantha and C. juncea; UBCEI = U. brizantha and C. ensiformis; PGCJI = P. glaucum and S = single system; UBS = Urochloa brizantha; PGS = Pennisetum glaucum; CJS = Crotalaria juncea; CES = C. juncea; PGCEI = P. glaucum and C. ensiformis; SV = spontaneous vegetation.

Table 5 .
Cover plant dry mass (DM) and cowpea yield (CY) as a function of different cover crops and crop cycles on a Latossolo Amarelo of the Amazon savanna, Boa Vista, Roraima State, Brazil, 2017.