scholarly journals Effective hydraulic conductivity and its relationship with the other attributes of Cerrado soils

2020 ◽  
Vol 24 (6) ◽  
pp. 357-363
Author(s):  
Edwaldo D. Bocuti ◽  
Ricardo S. S. Amorim ◽  
Luis A. Di L. Di Raimo ◽  
Wellington de A. Magalhães ◽  
Emílio C. de Azevedo
Keyword(s):  
Hydraulic Conductivity ◽  
Sandy Loam ◽  
Aggregate Stability ◽  
Stability Index ◽  
Water Infiltration ◽  
Total Carbon ◽  
Total Carbon Content ◽  
Mato Grosso ◽  
Effective Hydraulic Conductivity ◽  
Physical Attributes

ABSTRACT The objective of this study was to determine the effective hydraulic conductivity of six areas located in the Cerrado region of Mato Grosso, Brazil, and to identify physical attributes of soils with potential for predicting effective hydraulic conductivity. The tests to determine the effective hydraulic conductivity were carried out in six areas, covering the textural classes sand, sandy loam and clay, and the following uses: pasture, Cerrado and agriculture. Particle size, sand fractionation, total carbon content, degree of clay flocculation, bulk density, macroporosity, microporosity, mean weight diameter, mean geometric diameter and aggregate stability index were determined. From the data, statistical analyses of contrasts were performed by the Kruskal - Wallis test, and simple Pearson’s correlation coefficient was determined between variables. The average values of effective hydraulic conductivity for the pasture, agriculture and Cerrado areas were 95.73, 27.83 and 48.31 mm h-1, respectively. Higher value of effective hydraulic conductivity was observed in the Pasture area point 2 when compared to the Agriculture area point 2, because the amount of clay determined in Agriculture area was approximately 16 times greater than that of the area Pasture point 2, conditioning lower water infiltration in the soil profile of the area Agriculture point 2. Among the physical attributes analyzed, those with the highest potential for Ke prediction were: clay, silt, sand (coarse, medium and fine), total carbon and aggregate stability index.

scholarly journals INFLUÊNCIA DA COMPACTAÇÃO E DO CULTIVO DE SOJA NOS ATRIBUTOS FÍSICOS E NA CONDUTIVIDADE HIDRÁULICA EM LATOSSOLO VERMELHO

Irriga ◽  
2003 ◽  
Vol 8 (3) ◽  
pp. 242-249 ◽  
Author(s):  
Amauri Nelson Beutler ◽  
José Frederico Centurion ◽  
Cassiano Garcia Roque ◽  
Zigomar Menezes de Souza
Keyword(s):  
Hydraulic Conductivity ◽  
Bulk Density ◽  
Soil Compaction ◽  
Soil Surface ◽  
Total Porosity ◽  
Soil Condition ◽  
Agricultural Science ◽  
Water Infiltration ◽  
Loose Soil ◽  
Physical Attributes

INFLUÊNCIA DA COMPACTAÇÃO E DO CULTIVO DE SOJA NOS ATRIBUTOS FÍSICOS E NA CONDUTIVIDADE HIDRÁULICA EM LATOSSOLO VERMELHO   Amauri Nelson BeutlerJosé Frederico CenturionCassiano Garcia RoqueZigomar Menezes de SouzaDepartamento de Solos e Adubos, Faculdade de Ciências Agrárias e Veterinárias, Universidade Estadual Paulista, Jaboticabal, SP. CEP 14870-000. E-mail: [email protected], [email protected]  1 RESUMO              Este estudo teve como objetivo determinar a influência da compactação e do cultivo de soja nos atributos físicos e na condutividade hidráulica de um Latossolo Vermelho de textura média. O experimento foi conduzido na Universidade Estadual Paulista – Faculdade de Ciências Agrárias e Veterinárias, Jaboticabal (SP). Os tratamentos foram: 0, 1, 2, 4 e 6 passadas de um trator, uma ao lado da outra perfazendo toda a superfície do solo, com quatro repetições. O delineamento experimental foi inteiramente casualizado para a condutividade hidráulica e, em esquema fatorial 5 x 2 para os atributos físicos. Foram coletadas amostras de solo nas faixas de profundidades de 0,02-0,05; 0,07-0,10 e 0,15-0,18 m, por ocasião da semeadura e após a colheita para determinação da densidade do solo, porosidade total, macro e microporosidade do solo. A condutividade hidráulica do solo foi determinada após a colheita. O tempo entre a semeadura e a colheita de soja foi suficiente para aumentar a compactação do solo apenas na condição de solo solto. A compactação do solo reduziu a condutividade hidráulica em relação a condição natural (mata) e a condição de solo solto, sendo que esta não foi reduzida, após a primeira passagem, com o aumento no número de passagens.  UNITERMOS: Densidade do solo, porosidade do solo, infiltração de água, soja.  BEUTLER, A. N.; CENTURION, J. F.; ROQUE, C. G.; SOUZA, Z. M. COMPACTION AND SOYBEAN GROW INFLUENCE ON PHYSICAL ATTRIBUTES AND  HYDRAULIC CONDUCTIVITY IN RED LATOSSOL SOIL   2 ABSTRACT  The purpose of this study was to determine the influence of compaction and soybean grow on physical attributes and hydraulic conductivity of a Red Latossol, medium texture soil. The experiment was carried out in the experimental farm at the Paulista State University  – Agricultural Science College, Jaboticabal – São Paulo state. The treatments were 0, 1, 2, 4 and 6 side-by-side tractor strides on the soil surface with four replications. The experimental design was completely randomized for hydraulic conductivity and a 5 x 2 factorial design for soil physical attributes. Soil samples have been collected at 0.02-0.05, 0.07-0.10 and 0.15-0.18 m depth at sowing season and after harvest in order to determine soil bulk density, total porosity, macro and micro porosity. Soil hydraulic conductivity was determined after harvest. The time period between the soybean sowing and harvesting was enough to increase soil compaction only in loose soil condition. Soil compaction reduced hydraulic conductivity compared to the natural (forest) and loose soil condition  KEYWORDS: Bulk density, soil porosity, water infiltration, soybean.

Influence of long-term feedlot manure amendments on soil hydraulic conductivity, water-stable aggregates, and soil thermal properties during the growing season

2018 ◽  
Vol 98 (3) ◽  
pp. 421-435 ◽  
Author(s):  
J.J. Miller ◽  
B.W. Beasley ◽  
C.F. Drury ◽  
F.J. Larney ◽  
X. Hao ◽  
...  
Keyword(s):  
Thermal Properties ◽  
Hydraulic Conductivity ◽  
Physical Properties ◽  
Wood Chip ◽  
Aggregate Stability ◽  
Soil Surface ◽  
Soil Physical Properties ◽  
Total Carbon ◽  
Soil Thermal Properties

Long-term application of feedlot manure to cropland may change the physical properties of soils. We measured selected soil (surface) physical properties of a Dark Brown Chernozemic clay loam where different amendments were annually applied for 15 (2013), 16 (2014), and 17 (2015) yr. The treatments were stockpiled (SM) or composted (CM) manure with either straw (ST) or wood-chip (WD) bedding applied at three rates (13, 39, and 77 Mg ha−1) and an unamended control. The effect of selected or all treatments on selected properties was determined in 2013–2015. These properties included field-saturated (Kfs) and near-saturated hydraulic conductivity or K(ψ), bulk density (BD), volumetric water content, soil temperature, soil thermal properties, and wet aggregate stability. The hypotheses that selected soil physical properties would improve more for treatments with greater total carbon in the amendments (SM > CM, WD > ST) was rejected. The exceptions were significantly (P ≤ 0.05) lower soil BD for SM than CM and WD than ST for certain dates, and lower soil thermal conductivity for WD than ST. Most soil physical properties generally had no response to 15–17 yr of annual applications of these feedlot amendments, but a few showed a positive response.

Soil structure and stability in the spermosphere of myxosdiaspore chia (Salvia hispanica L.)

Soil Research ◽  
2019 ◽  
Vol 57 (6) ◽  
pp. 546 ◽  
Author(s):  
Mariana Amato ◽  
Rocco Bochicchio ◽  
Giacomo Mele ◽  
Rosanna Labella ◽  
Roberta Rossi
Keyword(s):  
Crop Production ◽  
Soil Structure ◽  
Sandy Loam ◽  
Aggregate Stability ◽  
Stability Index ◽  
Computer Assisted ◽  
Salvia Hispanica ◽  
Structure And Stability ◽  
Micro Tomography ◽  
Salvia Hispanica L

Mucilage produced by myxodiaspores has been mainly studied for its role in seed ecology. This work investigates changes due to mucilage in soil structure and stability in the spermosphere of the myxodiaspore crop chia (Salvia hispanica L.). In sandy-loam (S) repacked soil sown with chia and subjected to wetting–drying (DW), Computer Assisted X-ray micro tomography showed that extrusion of a mucilage capsule formed a pore of volume twice that of the seed, surrounded by a shell of particles with higher porosity and lower pore size than the bulk soil. In three soils (S; loam, L; and clay-loam, C) the aggregate stability index to wet sieving (Stw) decreased with one and two DW cycles. Application of 2% w/w mucilage increased Stw before and after DW, from 29% in C to more than 60-fold in S. Mucilage-amended samples after DW had higher or equal Stw compared with unamended soil before DW. Soil retained at the surface of hydrated diaspores exposed to water flow changed with soil texture (11.3, 90.5 and 91.7mg on each hydrated seed for S, L and C respectively) and chia genotype (6.7, 9.9 and 12.8mg per hydrated seed in BC and G8 long-day flowering mutants and commercial Black chia respectively). Our results showed that myxodiaspores affected soil structure by providing a microenvironment of altered porosity and high stability around the mucilage capsule extruded by the hydrated seed. This finding characterises a transient but crucial time of crop production around sowing when physical properties of soil surrounding seeds are relevant to stability, germination and plant–microorganism relations.

scholarly journals EFEITO DO CULTIVO DA CANA-DE-AÇÚCAR NA ESTABILIDADE DE AGREGADOS E NA CONDUTIVIDADE HIDRÁULICA DO SOLO

Irriga ◽  
2005 ◽  
Vol 10 (2) ◽  
pp. 116-122 ◽  
Author(s):  
Gilton Bezerra de Góes ◽  
Thiago Claudino Greggio ◽  
José Frederico Centurion ◽  
Amauri Nelson Beutler ◽  
Itamar Andrioli
Keyword(s):  
Hydraulic Conductivity ◽  
Sugar Cane ◽  
Aggregate Stability ◽  
Saccharum Officinarum ◽  
Natural Vegetation ◽  
Native Vegetation ◽  
Soil Aggregate Stability ◽  
Randomized Design ◽  
Physical Attributes ◽  
The Stability

EFEITO DO CULTIVO DA CANA-DE-AÇÚCAR NA ESTABILIDADE DE AGREGADOS E NA CONDUTIVIDADE HIDRÁULICA  DO SOLO  Gilton Bezerra de Góes;  Thiago Claudino Greggio;  José Frederico Centurion; Amauri Nelson Beutler; Itamar Andrioli Departamento de Solos e Adubos, Faculdade de Ciências Agrárias e Veterinárias, Universidade Estadual Paulista, Jaboticabal, SP.   1 RESUMO Para o cultivo de cana-de-açúcar ocorre intenso revolvimento do solo durante as operações de preparo para o plantio e à adubação.  Este estudo objetivou avaliar a estabilidade de agregados e a condutividade hidráulica de um Latossolo Vermelho distroférrico sob cana-de-açúcar com diferentes idades e sob vegetação natural. O experimento foi realizado em Jaboticabal, SP. Os sistemas de uso foram: solo sob mata natural (M), solo sob cana-de-açúcar de 1 ano (C1), sob cana-de-açúcar de 3 anos (C3) e sob cana-de-açúcar de 7 anos (C7). Para avaliação da estabilidade de agregados utilizou-se um delineamento inteiramente casualizado em parcela subdividida, com seis repetições, nas camadas de 0-10, 10-20, 20-30 e 30-40 cm; e para avaliação da condutividade hidráulica, o delineamento foi o inteiramente casualizado, com cinco repetições, na profundidade de 20 cm. Os sistemas de uso do solo com cana-de-açúcar reduzem a estabilidade de agregados e a condutividade hidráulica saturada em relação à mata nativa. UNITERMOS: atributos físicos, Saccharum officinarum.  GÓES, G.B.; GREGGIO, T.C.; CENTURION, J.F.; BEUTLER, A.N.; ANDRIOLI, I.  EFFECT OF SUGAR CANE CULTIVATION ON  SOIL AGGREGATE STABILITY AND HYDRAULIC CONDUCTIVITY  2 ABSTRACT For sugar cane (Saccharum officinarum) cultivation, the soil is intensively revolved during planting and fertilization tillage. Thus, this study aimed to evaluate the stability of aggregated soil and hydraulic conductivity in Oxisol soil under different age sugar cane and natural vegetation. The experiment was carried out in Jaboticabal, SP, Brazil. The systems of soil uses were the following ones: soil under natural vegetation (M), soil under 1-year sugar cane (C1), soil under 3-year sugar cane (C3) and under 7-year sugar cane (C7). A completely random design with subdivided plots and 6 replications were used in layers of 0-10 cm, 10-20 cm, 20-30 cm and 30-40 cm to evaluate the stability of aggregated soil; for hydraulic conductivity, an entirely randomized design and 5 replications were used at the depth of 20 cm. The systems of soil uses for sugar cane cultivation reduced the stability of aggregated soil and saturated hydraulic conductivity in relation to native vegetation. KEYWORDS: Physical attributes, Saccharum officinarum.

scholarly journals Land-use change effect on the hydro-dynamic characteristics of soil in the Brazilian semi-arid region

2020 ◽  
Vol 15 (2) ◽  
pp. 1
Author(s):  
Willames Albuquerque Soares ◽  
Simone Rosa da Silva ◽  
José Romualdo de Sousa Lima
Keyword(s):  
Hydraulic Conductivity ◽  
Arid Region ◽  
Soil Structure ◽  
Water Infiltration ◽  
Natural Soil ◽  
Forage Crops ◽  
Hydrodynamic Processes ◽  
Physical Attributes ◽  
Semi Arid Region ◽  
Semi Arid

 The search for better living conditions has led the residents of the Brazilian semi-arid region to plant forage crops, leading to a gradual decrease in the native vegetation (Caatinga) of this region. The effects caused by the replacement of Caatinga with palm, for example, have been little studied, especially with regard to the physical and hydraulic properties of the soil. The objective of this study was to compare the physical-hydraulic characteristics of a litholic neosol in two areas having different vegetation cover: one area cultivated with forage palm (O. ficus-indica) and the other covered by native Caatinga. Differences in soil structure, especially in porosity, between the natural and cultivated soils were observed to control the hydrodynamic processes, resulting in changes in water retention curves and hydraulic conductivity. Natural soil presents low values of hydraulic conductivity when compared to those of cultivated soil. This increase is probably due to soil management required for forage palm cultivation. The natural soil structure, characterized by relatively low saturated hydraulic conductivity values, presents an infiltrability that favors surface runoff. Human activities in the study area have promoted changes in the soil’s physical attributes, decreasing density and increasing porosity. Consequently, there is an increase in water infiltration into the soil and a reduction of runoff in cultivated areas, confirming results obtained in previous studies.

scholarly journals Effect of domestic greywater reuse for irrigation on soil physical and chemical characteristics and tomatoes growth.

2021 ◽  
Vol 115 (2) ◽  
pp. 51-63
Author(s):  
Guillaume Nyagatare ◽  
Christian Shingiro ◽  
Claire Nyiranziringirimana
Keyword(s):  
Hydraulic Conductivity ◽  
Sandy Loam ◽  
Tap Water ◽  
Block Design ◽  
Aggregate Stability ◽  
Growth Effect ◽  
Chemical Characteristics ◽  
Soil Hydraulic Conductivity ◽  
Soil Hydraulic ◽  
Physical And Chemical

This study aimed at determining the effect of laundry greywater on the growth of tomatoes and physical and chemical properties of a sandy loam Perrox in the Eastern province of Rwanda, Kayonza district, Mwiri sector. The experimental design consisted of plots planted with tomatoes (Lepersicon Esculantum) in a randomized complete block design with three replications and four treatments. Treatment 1: Tomatoes irrigated with pure greywater; Treatment 2: Tomatoes irrigated with a mixture of tap water and greywater at 1:1 ratio; Treatment 3: Alternation of greywater and tap water in a consecutive manner; and Treatment 4: only tap water serving as a control. Results showed that the following soil chemical parameters were significantly increased with greywater application: pH, EC, Av P, Na and SAR. Conversely, soil concentration in Mg and Ca significantly decreased with increase in greywater application. With the exception of soil bulk density, other measured physical properties such as soil hydraulic conductivity, aggregate stability and porosity were significantly reduced with greywater application. The highest values for soil hydraulic conductivity, aggregate stability and porosity were found for soil irrigated with tap water which ranged between 1.01 to 2.1 times higher than that of greywater, mixed or alternated with tap water. The alternate application of greywater and tap water did not affect significantly the stem height and weight of tomatoes. We concluded that the absence of positive growth effect of application of greywater was due to low concentration in essential plant nutrients in greywater, and induced adverse effects on soil chemical, physical, and biological properties. However, alternate application of the greywater and tap water preserved approximately the same soil physico-chemical characteristics as with application of tap water. Thus, among the irrigation treatments involving greywater, the latter should be considered as the most environmentally friendly. We propose combination of greywater with various forms of composts as the one of the most promising investigations on the reuse of greywater in irrigation.

Transport of soluble organic and inorganic carbon in sandy soils under nitrogen fertilization

1999 ◽  
Vol 79 (2) ◽  
pp. 303-310 ◽  
Author(s):  
F. L. Wang ◽  
A. K. Alva
Keyword(s):  
Nitrogen Fertilization ◽  
Inorganic Carbon ◽  
Average Rate ◽  
Sandy Soils ◽  
Water Soluble ◽  
Total Carbon ◽  
Total Carbon Content ◽  
Water Soluble Organic Carbon ◽  
Isobutylidene Diurea ◽  
Leaching Condition

Leaching of water soluble soil carbon plays an important role in downward transport of soil nutrients and pollutants and may be influenced by soil and management factors. We examined the leaching of water soluble carbon from two sandy soils under nitrogen fertilization by adapting an intermittent leaching-incubation technique using packed soil columns (94 × 10 cm). After 30 d, cumulative amounts of water-soluble organic carbon (SOC) leached from the Candler and Wabasso sand for various treatments in mg C column−1 were: 77 and 302 (NH4NO3), 64 and 265 (control), and 45 and 239 (isobutylidene diurea, IBDU), respectively. The IBDU and NH4NO3 treatments increased the leaching of water-soluble inorganic carbon (SIC), which ranged from 2 to 38 mg C column−1 over 30 d. At the end of eight cycles of leaching/incubation, the total carbon content increased at depth (control and NH4NO3 treatment) in the Candler sand, but decreased in the Wabasso sand. In the first leaching event, the average rate of SOC leaching from the Wabasso sand was 26 mg C column−1 d−1 which dropped rapidly to about 5 mg C column−1 d−1 towards the end of the experiment. The rate of SOC leaching from the Candler sand was much lower (<8 mg C column−1 d−1) than the rate of SOC leaching from the Wabasso sand. Compared with the unamended treatments, application of NH4NO3 increased and IBDU decreased the leaching of SOC in both soils. These effects of N application were considerable during the initial two to three leaching events only. Our results suggest that the initial rainfalls that follow a dry period may be critical for transporting SOC from the upper layer of these sandy soils. Key words: C leaching, sandy soil, intermittent leaching condition, isobutylidene

scholarly journals Characteristics of Liparis loeselii (L.) Rich. populations in selected Natura 2000 areas in eastern Poland

2020 ◽  
Vol 55 (3) ◽  
pp. 151-162
Author(s):  
Danuta Urban ◽  
Joanna Sender ◽  
Ewelina Tokarz ◽  
Andrzej Różycki
Keyword(s):  
Natura 2000 ◽  
Total Carbon ◽  
Habitat Conditions ◽  
Total Carbon Content ◽  
Poor Fen ◽  
Calcareous Fen ◽  
Liparis Loeselii ◽  
The Individual ◽  
Insight Into

AbstractIn view of the sensitivity of Liparis loeselii to changes in habitat conditions, we carried out a study with the aim to monitor population numbers, identify the individual features of the Liparis loeselii population, analyse habitat conditions, identify threats and propose conservation measures to preserve the species. The investigations were conducted in seven unmanaged objects located in three Natura 2000 areas in eastern Poland. The results of this study provide a new insight into Liparis loeselii ecology. The analysed populations inhabited some habitat types: extremely poor fen, transitional mire, rich fen, calcareous fen, spring-fed fen. The content of nutrients was similar in all the habitats. A CCA analysis revealed that the total carbon content, pH, and redox potential of the substrate determine differences between the habitats analysed. Juvenile individuals represented a maximum of 12% of the analysed populations and were the least abundant group of these plants. The flowering was primarily influenced by hydrological conditions. Based on the long-term observations reported in this article, it can be assumed that the species stands a chance of surviving at the localities analysed, provided that the habitat conditions do not change dramatically.

scholarly journals Treated wastewater irrigation effects on soil hydraulic conductivity and aggregate stability of loamy soils in Israel

2015 ◽  
Vol 63 (1) ◽  
pp. 47-54 ◽  
Author(s):  
Karsten Schacht ◽  
Bernd Marschner
Keyword(s):  
Hydraulic Conductivity ◽  
Chemical Properties ◽  
Aggregate Stability ◽  
Treated Wastewater ◽  
Soil Aggregate Stability ◽  
Irrigation Effects ◽  
Physical And Chemical ◽  
The Impact

Abstract The use of treated wastewater (TWW) for agricultural irrigation becomes increasingly important in water stressed regions like the Middle East for substituting fresh water (FW) resources. Due to elevated salt concentrations and organic compounds in TWW this practice has potential adverse effects on soil quality, such as the reduction of hydraulic conductivity (HC) and soil aggregate stability (SAS). To assess the impact of TWW irrigation in comparison to FW irrigation on HC, in-situ infiltration measurements using mini disk infiltrometer were deployed in four different long-term experimental orchard test sites in Israel. Topsoil samples (0-10 cm) were collected for analyzing SAS and determination of selected soil chemical and physical characteristics. The mean HC values decreased at all TWW sites by 42.9% up to 50.8% compared to FW sites. The SAS was 11.3% to 32.4% lower at all TWW sites. Soil electrical conductivity (EC) and exchangeable sodium percentage (ESP) were generally higher at TWW sites. These results indicate the use of TWW for irrigation is a viable, but potentially deleterious option, as it influences soil physical and chemical properties.

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