Roots of Perennial Grasses in the Recovery of Soils Degraded by Coal Mining in Southern Brazil

Revegetation of degraded soils is crucial to prevent erosion and improve soil structure and quality. We aimed to elucidate the role of the root system of grasses on the reclamation of a soil constructed after coal mining. In Candiota city, in Brazil, perennial grasses (Hemarthria, Paspalum, Cynodon, and Brizantha) were cultivated for 103 months, when soil samples were collected from 0.00–0.30 m layer. The root development of these species substantially decreased in depth, reflecting soil restrictive conditions, as high soil penetration resistance, especially below 0.10 m, assigned to the use of heavy machinery during soil construction. Below 0.10 m depth, fine and flattened roots were observed, which penetrated through the cracks of compacted soil layers. Regardless of the soil layer, all plant species had a greater proportion of roots 0.50 mm diameter class, averaged 92 and 8%, respectively. Below 0.10 m depth, Brizantha increased the proportion of roots >0.50 mm diameter class, while the other grasses increased the proportion of roots <0.49 mm diameter class. The highest root density, volume, and length observed for Brizantha along the soil profile indicate its high potential to improve physical attributes and therefore the quality of the constructed soil

Persistência dos efeitos da escarificação sobre a compactação de Nitossolo sob plantio direto em região subtropical úmida

The objective of this work was to evaluate the persistence of chiseling effects on the compaction of a Ferralic Nitisol (Rhodic), under no‑till (NT), in the Brazilian humid subtropical region. The experiment was carried out in randomized complete blocks, with four replicates and six treatments, consisting of the time that the soil was kept under NT after chiseling: continuous NT for 24 months, after chiseling in September 2009; continuous NT for 18 months, after chiseling in March 2010; continuous NT for 12 months, after chiseling in September 2010; continuous NT for six months, after chiseling in March 2011; crop planted right after soil chiseling, in September 2011; and continuous NT, without chiseling (control). The species cultivated in the area were: corn in the 2009/2010 growing season; wheat in 2010; soybean in the 2010/2011 growing season; rye in 2011; and corn in the 2011/2012 growing season. Treatment effects were assessed by soil physical parameters and by morphological and productive parameters of the corn crop in the 2011/2012 growing season. The chiseling of Nitisol under no‑till in a humid subtropical region does not increase corn grain yield, and its effects on soil structure do not last longer than 18 months.O objetivo deste trabalho foi avaliar a persistência dos efeitos da escarificação sobre a compactação de Nitossolo Vermelho, manejado sob plantio direto (PD), na região subtropical úmida do Brasil. O experimento foi realizado em blocos ao acaso, com quatro repetições e seis tratamentos, constituídos pelo tempo de manutenção do solo sob PD após escarificação: PD contínuo por 24 meses após escarificação, realizada em setembro de 2009; PD contínuo por 18 meses após escarificação, realizada em março de 2010; PD contínuo por 12 meses após escarificação, realizada em setembro de 2010; PD contínuo por seis meses após escarificação, realizada em março de 2011; plantio realizado em solo recém escarificado, em setembro de 2011; e PD contínuo e sem escarificação (testemunha). As espécies cultivadas na área foram: milho, safra 2009/2010; trigo, em 2010; soja, safra 2010/2011; centeio, em 2011; e milho, safra 2011/2012. Os efeitos dos tratamentos foram avaliados a partir de parâmetros físicos do solo e de parâmetros morfológicos e produtivos da cultura do milho, na safra 2011/2012. A escarificação do Nitossolo sob plantio direto, em região de clima subtropical úmido, não aumenta a produtividade de grãos de milho, e os seus efeitos sobre a estrutura do solo não persistem por mais de 18 meses

Atributos químicos e biológicos de um solo de várzea afetados pela sistematização do terreno

The objective of this work was to evaluate the relationship between soil chemical and biological attributes and the magnitude of cuts and fills after the land leveling process of a lowland soil. Soil samples were collected from the 0–0.20 m layer, before and after leveling, on a 100 point grid established in the experimental area, to evaluate chemical attributes and soil microbial biomass carbon (MBC). Leveling operations altered the magnitude of soil chemical and biological attributes. Values of Ca, Mg, S, cation exchange capacity, Mn, P, Zn, and soil organic matter (SOM) decreased in the soil profile, whereas Al, K, and MBC increased after leveling. Land leveling decreased in 20% SOM average content in the 0–0.20 m layer. The great majority of the chemical attributes did not show relations between their values and the magnitude of cuts and fills. The relation was quadratic for SOM, P, and total N, and was linear for K, showing a positive slope and indicating increase in the magnitude of these attributes in cut areas and stability in fill areas. The relationships between these chemical attributes and the magnitude of cuts and fills indicate that the land leveling map may be a useful tool for degraded soil recuperation through amendments and organic fertilizers.O objetivo deste trabalho foi avaliar a relação entre os atributos químicos e biológicos do solo e as magnitudes de cortes e aterros após sistematização de um solo de várzea. Foram coletadas amostras de solo na camada de 0–0,20 m, antes e depois da sistematização, em uma malha de 100 pontos estabelecida na área experimental, para avaliar os atributos químicos do solo e o carbono da biomassa microbiana (CBM). A sistematização alterou a magnitude dos atributos químicos e biológicos do solo. Valores de Ca, Mg, S, capacidade de troca catiônica, Mn, P, Zn e matéria orgânica do solo (MOS) diminuíram no perfil do solo, enquanto os de Al, K e CBM aumentaram após a sistematização. A sistematização reduziu em 20% o conteúdo médio de MOS na camada de 0–0,20 m. A maior parte dos atributos químicos não apresentou relação com as magnitudes de corte e aterro. A relação foi quadrática para MOS, P e N total, e linear para K, mostrando inclinação positiva e aumento das magnitudes destes atributos em áreas de corte e estabilidade em áreas de aterro. As relações entre estes atributos químicos e as magnitudes de cortes e aterro indicam que o mapa de sistematização pode ser uma ferramenta útil para a recuperação de solos degradados por meio da aplicação de corretivos e fertilizantes orgânicos

Condição física e desenvolvimento radicular de gramíneas em solo construído após mineração de carvão

The objective of this work was to evaluate the root development of the physical condition and the potential of agricultural use of a constructed minesoil after coal mining, besides the root development of tropical grasses in this soil, considering different revegetation periods. The soil was constructed in early 2003, and the experiment was installed in November/December 2007. Soil physical condition was evaluated in plots vegetated with perennial grasses such as Urochloa humidicola, Panicum maximum, and U. brizantha. In July 2012, disturbed and undisturbed soil samples were taken for determining physical and chemical attributes in the 0.00–0.10, 0.10–0.20, and 0.20–0.30-m soil layers. Soil monoliths were collected for characterizing the root system. After 58 months of revegetation, the physical condition of the constructed minesoil is still inadequate to an agricultural use that requires intensive soil management. Among the evaluated layers, only the 0.00–0.10-m layer provides conditions for the soil to function properly in the ecosystem. Urochloa brizantha was more promising for the recovery of soil structure in the 0.00–0.10-m soil layer, and root density was the most sensitive attribute to distinguish the potential development of the different species in this layer.O objetivo deste trabalho foi avaliar a condição física e a potencialidade de uso agrícola de um solo construído após mineração com carvão, além do desenvolvimento radicular de gramíneas tropicais nesse solo, tendo‑se considerado diferentes períodos de revegetação. O solo foi construído no início de 2003, e o experimento instalado em novembro/dezembro de 2007. A condição física do solo construído foi avaliada nas parcelas ocupadas por gramíneas perenes, como Urochloa humidicola, Panicum maximum e U. brizantha. Em julho de 2012, foram coletadas amostras de solo com estrutura preservada e não preservada para a determinação dos atributos físico-químicos, nas camadas de 0,00–0,10, 0,10–0,20 e 0,20–0,30 m. Monólitos de solo foram coletados para caracterização do sistema radicular das diferentes gramíneas. Após 58 meses de revegetação, a condição física do solo construído ainda é inadequada ao uso agrícola que envolva práticas mais intensivas de manejo de solo. Entre as camadas avaliadas, somente a de 0,00–0,10 m fornece condições para que o solo cumpra suas funções no ecossistema. Urochloa brizantha mostra-se mais promissora para a recuperação da estrutura do solo na camada de 0,00–0,10 m, e a densidade radicular foi o atributo mais sensível para a diferenciação do desenvolvimento potencial das diferentes espécies nesta camada

Reclamation of Soils Degraded by Surface Coal Mining

The largest Brazilian coal mine, called Candiota mine, is located in South Brazil, with an estimated reserve about 1.2 billion tons. Since late 2003, an experiment located at a reclaimed site in a coal mining area was conducted, in which a research group from the Federal University of Pelotas has been conducting a long-term experiment on soil quality with different plants species, such as Hemarthria altissima, Paspalum notatum cv. Pensacola, Cynodon dactylon cv. Tifton, and Urochloa brizantha. After 8.6 years of revegetation, soil samples at 0.20 depth were collected in minesoil and natural soil to determine physical attributes, and the organic carbon content. After 10.9 years of revegetation, soil samples at 0.10 m depth were collected to determine the biological attributes. According to the research results, it can be seen that the recovery of minesoil was more effective after 8.6 years of revegetation only in the physical condition up to 0.10 m depth. However, all soil physical attributes and organic matter content are still below the levels observed in the natural soil. The biological attributes after 10.9 years of revegetation have not yet been sufficient to restore a mites and springtails population close to the natural soil

Impact of Revegetation on Ecological Restoration of a Constructed Soil in a Coal Mining in Southern Brazil

The main problems in the constructed soils are the generation of acid mine drainage promoted by the presence of coal debris in the overburden layer and the compaction of the topsoil promoted by the machine traffic when the material used in the overburden cover is more clayey. This book chapter aimed to show an overview of the impact of more than a decade of revegetation with different perennial grasses on the chemical, physical, and biological quality of constructed soil after coal mining. The study was carried out in a coal mining area, located in southern Brazil. The soil was constructed in early 2003 and the perennial grasses, Hemarthria altissima; Paspalum notatum cv. Pensacola; Cynodon dactylon cv Tifton; and Urochloa brizantha; were implanted in November/December 2003. In 11.5, 17.6 and 18 years of revegetation soil samples were collected and the chemical, physical, and biological attributes were determined. Our results show that liming is an important practice in the restoration of these strongly anthropized soils because this positively impacts the plants’ development, facilitating the roots system expansion. Biological attributes such as soil fauna and the microorganism’s population are the attributes that possibly takes longer to establish itself in these areas

Physical Quality of Soils in a Toposequence of a Forest Fragment under Livestock Activity in a Watershed in South Brazil

The conservation of native forests is fundamental to the preservation of hydric resources in the landscape. The use of animals in forest fragments has resulted in degradations in the soil, resulting in the grating of these. Thus, soil classes were studied and physical parameters of forest soils were evaluated in areas without and with cattle grazing in the “Arroio Pelotas” watershed, Pelotas, Rio Grande do Sul, extreme south of Brazil. The results were submitted to statistical analysis with the Kruskal–Wallis nonparametric test with a significance level of 5%. The means of the physical parameters of soil in the same toposequence and layers with and without the presence of livestock were compared. By analyzing soil physical attributes (density, macroporosity, and microporosity) it can be seen that the structural quality of the soil is affected by the access of animals inside the forest fragments, especially in the upper layer of the soil (0–5 cm deep). In forest fragments without access to animals, the physical structure of the soil presented the best conditions of macroporosity and, consequently, greater protection of nutrients, microorganisms, and water resources. Therefore, it is concluded that conservation by the isolation of protective forests in rural property planning benefits the quality of forest soils