Changes in physical properties and organic carbon of a Kandiudox fertilized with manure

Andrade, Andréia Patrícia; Rauber, Luiz Paulo; Mafra, Álvaro Luiz; Baretta, Dilmar; Rosa, Márcio Gonçalves da; Friederichs, Augusto; Mafra, Maria Sueli Heberle; Casara, Ana Cláudia

doi:10.1590/0103-8478cr20150540

Cited by 16 publications

(11 citation statements)

References 13 publications

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“…The organic matter present in the liquid swine waste is predominantly composed of labile organic carbon (ANGERS et al, 2010) and its annual application throughout this growing period can contribute to the increase and maintenance of this soil organic matter compartment. Unlike the results observed in this study, Andrade et al (2016) and Rauber et al (2017) values did not vary between the areas of cultivation, it can be inferred that the main compartment of organic matter being influenced by the management is the POC.…”

Section: Discussioncontrasting

confidence: 99%

“…When evaluating the dynamics of total C, POC and MAOC in a Nitossolo (Ultisol) in Concórdia-SC, in an area of yerba mate with 20 years of successive cultivation, Rauber et al (2017) found smaller amounts of these fractions when compared to an adjacent native forest. Similarly, Andrade et al (2016) evaluated the effect of the application of organic fertilizers in areas with 20 years of yerba mate monoculture in a Nitossolo Vermelho (Ultisol) and also found lower contents of C, POC and MAOC compared to a native forest.…”

Section: Introductionmentioning

confidence: 99%

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Soil Organic Matter in Areas Under Yerba Mate Cultivation and Swine Waste Application

Pereira

Guareschi

Pinto

et al. 2021

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Carbon and nitrogen contents, as well as their chemical fractions (humic acid - HAF, fulvic acid - FAF, humin - HUM) and particle-size fractions (particulate organic carbon - POC, mineral-associated organic carbon - MAOC) of organic matter were evaluated in areas cultivated with yerba mate (Ilex paraguariensis) with 35 (E35) and 45 (E45) consecutive years of cultivation, in addition to a native forest area (NF), taken as reference. The soils of the study area were classified as Cambissolo Háplico (Inceptisol). Soil samples were collected at depths of 0.0-0.05, 0.05-0.10, 0.10-0.20 and 0.20-0.40 cm. A completely randomized design in split plots (3 areas and 4 depths) with 4 replicates was used. The E45 area, due to the longer cultivation time and the addition of organic fertilizer, had higher TOC, N and POC contents in comparison to the E35 area, with similar values of these attributes being observed in the forest area at some depths. The most stable carbon fractions (MAOC and HUM) did not vary between cultivated areas (E35 and E45); however, there were reductions of 25 and 14% (HUM 0-5 cm) and 12 and 21% (MAOC 5-10 cm) in these fractions, respectively, in comparison to the native forest. There was no difference between the evaluated areas for FAF, but HAF values were higher in the native forest area than in the cultivated areas.

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Section: Discussioncontrasting

confidence: 99%

Section: Introductionmentioning

confidence: 99%

Soil Organic Matter in Areas Under Yerba Mate Cultivation and Swine Waste Application

Pereira

Guareschi

Pinto

et al. 2021

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“…The samples were used to determine the soil bulk density (Bd), the total porosity (Tp), and the macropore (Ma) and micropore (Mi) spaces by measuring the water saturation of the rings, draining them on a tension table under a matric potential of 6 kPa, and drying the samples at 105°C (EMBRAPA, 1997). The biopore volume (Bio) was quantified by withdrawing water from the saturated rings on the tension table under a matric potential of 1 kPa (ANDRADE et al, 2016).…”

Section: Methodsmentioning

confidence: 99%

Study of soil physical properties and water infiltration rates in different types of land use

Santos

Barbosa

Bertol

et al. 2018

SCA

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Studying the changes in soil properties caused by different land uses allows measures to be adopted that will reduce the risk of future negative effects. The aim of this study was to evaluate soil physical properties and quantify water infiltration for different types of land use in the Santa Catarina Plateau of southern Brazil. The research was conducted on a 1,200 ha rural property. The land use types selected were natural forest (NF), planted pine (PP), crop-livestock integration (CLI), and burned natural rangeland (BR). A sample survey was carried out in nine different areas for each land use. Samples were collected from four soil layers and the soil bulk density (Bd), total porosity (Tp), and macropore (Ma), micropore (Mi), and biopore (Bio) volumes were measured. Water infiltration tests were performed to obtain the initial (ii) and final (fi) water infiltration rates into the soil, and the total amount of water that had infiltrated the soil (Ti). In NF, Bd was lower and Tp was higher than in other types of land use. The forest vegetation (NF and PP) had higher Ma and Bio volumes in the superficial layers of the soil. Water infiltration was markedly different between land use types. The NF had the highest ii, fi, and Ti values followed by PP, whereas the CLI and BR areas had drastically lower infiltration parameters with BR having the lowest values. The variables ii, fi, and Ti correlated positively with Tp, Ma, and Bio, but negatively with Bd. ResumoO estudo das modificações nos atributos do solo provocadas pela forma de utilização das terras possibilita a adoção de medidas que reduzam riscos de futuros impactos. A pesquisa teve por objetivos quantificar atributos físicos do solo e a infiltração de água em diferentes modalidades de uso da terra no Planalto Sul Catarinense. O estudo foi conduzido em propriedade rural de 1.200 ha, onde foram selecionadas áreas sob floresta natural (FN), plantio de pinus (PP), integração lavoura-pecuária (ILP) e campo natural pastejado e submetido à queima (CN). Para isso, realizou-se levantamento amostral em nove glebas distintas para cada tipo de uso. Foram coletadas amostras de solo em quatro camadas para determinação da densidade do solo (Ds), porosidade total (Pt), macroporos (Ma), microporos (Mi) e bioporos (Bio).Testes de infiltração de água no solo foram realizados para obtenção das taxas de infiltração inicial (ii) e final (if) e da lâmina total infiltrada (It). Na FN a Ds é menor e a Pt maior do que nos demais tipos de uso da terra. A vegetação florestal (FN e PP) se destaca com maiores volumes de Ma e Bio nas camadas superficiais do solo. A infiltração de água apresenta diferenças acentuadas entre os tipos de uso. A FN tem maiores valores de ii, if e It, seguida pelo PP, enquanto CN e ILP tem redução drástica nos parâmetros de infiltração, com menores valores no CN. As variáveis ii, if e It correlacionam-se positivamente com Pt, Ma e Bio e negativamente com Ds. Palavras-chave: Qualidade do solo. Lavoura, pecuária e floresta. Permeabilidade do solo.

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“…Is there any time after which it starts to be harmful to soils? There are many studies that have shown an improvement in soil quality after at least 10 years of treatment, e.g., Asada et al [27] in Japan (13 years); Loss et al [28] in Brazil (10 years); and Andrade et al [29] and Rodrigues de Melo et al [30], also in Brazil (20 years and 9 years with chicken manure, respectively).…”

Section: Introductionmentioning

confidence: 99%

Effects of Applying Liquid Swine Manure on Soil Quality and Yield Production in Tropical Soybean Crops (Paraná, Brazil)

et al. 2019

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Brazil is one of the main producers of pork meat in the world. It is well-known that the agricultural sector is a key component of the economic development of this country, where super-intensive fields are only competitive in the globalized market. For the farmers, the application of swine manure to fertilize the soil can increase the yearly income, but it also may cause serious environmental problems related to soil health and soil quality. In this research, we assessed the effects of applying liquid swine manure in a tropical soybean (Glycine max) plantation to better understand when this technique stops being effective and starts causing a threat to soil health and quality. Therefore, we compared values of several soil properties and the soybean yield on treated fields at 10 random points belonging to 7 different plots that were treated with the liquid swine manure over a period ranging from 0 to 15 years. The results showed a positive linear trend in soybean production from 2.45 to 3.08 Mg ha−1 yr−1. This positive trend was also recorded for some key soil parameters such as porosity and exchangeable cations content (Ca, Mg, K, and Al). Additionally, positive effects were also found for organic matter content after 10 years of application. Our findings suggest that the use of liquid swine manure has a positive effect on soybean yield and improves soil quality, particularly on mixed farms where pigs are intensively raised nearby cultivated fields.

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Changes in physical properties and organic carbon of a Kandiudox fertilized with manure

Abstract: ABSTRACT

Cited by 16 publications

References 13 publications

Soil Organic Matter in Areas Under Yerba Mate Cultivation and Swine Waste Application

Soil Organic Matter in Areas Under Yerba Mate Cultivation and Swine Waste Application

Study of soil physical properties and water infiltration rates in different types of land use

Effects of Applying Liquid Swine Manure on Soil Quality and Yield Production in Tropical Soybean Crops (Paraná, Brazil)

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