The Effect of Soil Management on Pore Size Distribution and Water Infiltration

Abstract Water infiltration into soil varies significantly with soil type and management practices. Management practices alter soil physical properties, such as porosity and pore size distribution, which play an important role in infiltration. This study was conducted to assess the effect of the long-term use of two different soil tillage systems (conventional, CT, and no-tillage, NT) on soil structure and water infiltration to understanding of the relationship between physical conditions induced by tillage and water infiltration. The experiments were carried out on a Humic Cambisol in southern Brazil from 1995 to 2016. Soil density, porosity, aggregate diameter and soil water infiltration were evaluated under conventional tillage right after one plowing and two subsequent discings (CT0), and six months after these tillage operations (CT6). The results show that different management systems affect differently soil physical properties and, thus, water infiltration. By mechanical mobilization CT brings about modifications in soil structure which promote an increase in total porosity and mesopority, and a decrease in soil microporosity. This in turn results in an increase in the proportion of larger pores in the plow layer and a decrease in soil density, but also in a decrease in aggregate stability. The CT0 measurements showed the highest infiltration rates which were up to 15 times greater than in the NT treatment. The higher infiltration rate in CT0 wears off with time, but in the CT6 measurements six months after tillage it was still 2 times higher than under NT. Tillage, at least initially, increases total porosity and mesoporosity, while at the same time decreasing microporosity. This results in a larger saturated hydraulic conductivity (K). An increase in total porosity alone does not necessarily increase K, if there is an increase in small pores at the cost of decreasing the number of larger pores.

Chemical Recovery of Degraded Soil and Consequence in the Cost of Corn Production

Abstract Improper management degrades the soil, decreases corn productivity and is reflected in the cost of production. The objective of this research was to evaluate the soil recovery in non-conservationist treatments after the change of management and cultivation to the conservation condition direct sowing, and compare these systems to consolidated direct seeding; This evaluation was based on the soil responsiveness to crop production and water erosion control, and based on the financial cost of soil recovery and corn production when soil management was converted from non-conservationist (tillage rotation - RT, minimum tillage - MT, conventional tillage - CT and bare soil - BS) to no-tillage (NT) condition, in a Humic Cambisol. The transition from managements to no-tillage occurred in 2015 year, after 27 years of conducting the preexisting managements. The chemical recovery was carried out with the application of limestone, phosphorus, and potassium. At the end of the research the yield of the corn crop, the cost of recovering the soil fertility and the cost of crop production were evaluated. Previous soil management influenced the cost of soil chemical recovery. The cost of production showed a financial loss for the previous treatments CT and BS, on the average of the three corn crops.

Transferência superficial de fósforo reativo potencialmente contaminante por chuvas simuladas intensas / Superficial loss of reactive phosphorus potentially contaminant by intense rainfall simulation

O fósforo naturalmente presente ou adicionado ao solo, dependendo da conjunção de fatores, pode desencadear uma situação de alto risco ambiental para os recursos hídricos de bacias hidrográficas. O objetivo deste trabalho foi quantificar a transferência na superfície do solo de algumas formas de fósforo reativo, originário da adubação fosfatada em solo sem cultivo e descoberto, transportado pelo escoamento superficial da água de chuvas. O experimento foi executado em Lages, SC, com duas repetições de campo, sob regime de chuvas intensas simuladas (64 mm h−1 durante 50 minutos). Os resultados apontam que o fósforo pode representar sério risco ambiental aos recursos hídricos das bacias, em diferentes escalas no tempo e no espaço, através das formas reativas de fósforo e suas diferentes maneiras de transporte.

Phosphorus is naturally present or added to the soil and, depending on the mix of factors, may trigger a high environmental risk to water resources in river basins. The aim of this study was to quantify the transfer for soil surface of some forms of reactive phosphorus originating from phosphorus fertilization on bare soil, carried by the runoff. The experiment was carried out in Lages, SC, Brazil, with two replications in the field under intense simulated rainfall (64 mm h−1 for 50 minutes). The results indicate that phosphorus may represent a serious environmental risk to water resources of basins at different scales in time and space, through the reactive forms of phosphorus and their different ways of transportation.

Atributos químicos de um Cambissolo Húmico após 12 anos sob preparo convencional e semeadura direta em rotação e sucessão de culturas / Chemical properties of a Humic Dystrudept after 12 years under conventional and no tillage with crop succession and rotation

O manejo adequado do solo é uma das bases para a sustentabilidade do sistema agrícola. O objetivo do estudo foi avaliar atributos químicos de um Cambissolo Húmico Alumínico após 12 anos em dois sistemas de preparo do solo, com rotação e sucessão de culturas. O experimento foi conduzido em Lages, SC, utilizando preparo convencional (PC) e semeadura direta (SD), sob rotação (r) e sucessão (s) de culturas. O delineamento experimental foi inteiramente casualizado com quatro repetições. As sequências de cultivo foram: feijão-pousio-milho-pousio-soja-pousio no PCr; milho-pousio no PCs; feijão-aveia-milho-nabo-soja-ervilhaca na SDr; e milho-ervilhaca na SDs. As amostras de solo foram coletadas nas camadas 0-2,5; 2,5-5; 5-10; e 10-20cm. Avaliou-se carbono orgânico total (COT), cálcio, magnésio, alumínio trocável, fósforo, potássio, nitrogênio total (NT) e pH em água. A SD aumentou os teores de COT e nutrientes em comparação ao PC, especialmente na camada superficial do solo. O cultivo de milho e ervilhaca em sucessão aumentou os teores de COT e NT na camada superficial do solo em comparação com a rotação sob semeadura direta.

Suitable soil management is one of the bases for sustainability in agricultural systems. The study aimed to evaluate chemical properties of a Humic Dystrudept for 12 years under two tillage systems, with crops rotation and succession. The experiment was carried out in Lages, SC, under conventional tillage (CT) and no-till (NT), with rotation (r) and succession (s) cropping systems, using crop sequences of beans-fallow-maize-fallow-soybean in CTr; maize-fallow in CTs; beans-oats-maize-fodder radish-soybean-vetch in NTr; and maize-vetch in NTs. The experimental design was completely randomized with four replicates. The soil samples were collected in the layers 0-2.5, 2.5-5, 5-10 and 10-20cm. The variables assessed were total organic carbon (TOC), calcium, magnesium, exchangeable aluminum, phosphorus, potassium, total nitrogen (TN) and water pH. The no-tillage system increased TOC and nutrient levels in comparison with conventional tillage, especially in the surface soil layer. Maize and vetch crop succession had higher TOC and TN contents in the surface soil layer compared to crop rotation under no-tillage.

Propriedades químicas e fauna do solo influenciadas pela calagem em sistema semeadura direta / Effects of liming on chemical properties and soil fauna in no-tillage system

Este trabalho objetivou avaliar o efeito da calagem e sua influência sobre atributos químicos e de fauna do solo em um Cambissolo sob sistema de semeadura direta. O experimento vem sendo conduzido em Lages, SC, desde maio de 2001. Os tratamentos foram: semeadura direta com calcário incorporado na dose de 1 SMP (SD-inc) e superficial nas doses de 1/5 SMP (SD-1/5sup) e 1/2 SMP (SD-1/2sup). Como padrão, utilizou-se solo sem cultivo e sem aplicação de calcário, e uma área de pastagem perene com calcário incorporado na dose de 1 SMP (PI-inc). O solo foi amostrado nas camadas de 0-5; 5-10; 10-20cm para análise de Ca2+, Mg+2, Al3+, pH em água e em CaCl2; e de 0-10cm para carbono orgânico total e fauna do solo. A aplicação superficial de calcário no sistema de semeadura direta na maior dose (1/2 SMP) elevou os teores de Ca2+ até 10cm de profundidade e de Mg+2 até a camada de 10 a 20cm. A abundância e a diversidade da fauna edáfica foram maiores nas áreas sob semeadura direta e pastagem, em relação ao solo sem cultivo, mostrando sensibilidade às alterações advindas do manejo do solo, mas sem correlação direta com as modificações químicas decorrentes da calagem.

This research was aimed at evaluating the effect of liming and its influence on chemistry and fauna properties of a Cambisol under no-tillage system. The experiment has been carried out in Lages, SC, southern Brazil, since May 2001. The treatments were: no-tillage with incorporated lime in the rate of 1 SMP (NT-inc); superficial liming in the rate of 1/5 SMP (NT-1/5sup), and 1/2 SMP (NT-1/2sup). As control treatment, bare soil without cultivation without lime application (BS), and plots with perennial pasture with incorporate lime in the rate of 1 SMP (Pp-inc) were used. Soil samples were collected in the layers of 0-5; 5-10; 10-20cm depth for analysis of Ca2+, Mg+2, Al3+, water and CaCl2 pH. Total organic carbon and soil fauna were analysed in the layer 0-10cm. The superficial liming in the no-tillage system in the highest rate (1/2 SMP) increased Ca2+ contents up to 10 cm depth and Mg+2 up to the layer of 10 to 20cm. The abundance and diversity of soil fauna were higher in cultivated plots under no-tillage and pasture, in relation to the bare soil, showing influences of soil management, but with no direct relation with chemical soil conditions created by liming.