scholarly journals ATRIBUTOS QUÍMICOS DE LATOSSOLO VERMELHO SUBMETIDO A DIFERENTES MANEJOS

FLORESTA ◽  
2015 ◽  
Vol 45 (2) ◽  
pp. 229
Author(s):  
Ludmila De Freitas ◽  
José Carlos Casagrande ◽  
Ivanildo Amorim de Oliveira ◽  
Milton Cesar Costa Campos
Keyword(s):  
Organic Matter ◽  
Management Practices ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Agricultural System ◽  
Native Forest ◽  
Continuous Cropping ◽  
Soil Layers ◽  
Aluminum Saturation ◽  
Potential Acidity

A retirada da vegetação natural para implantação de sistema agrícola pode provocar desequilíbrios no solo, conforme o sistema de manejo empregado. Com o objetivo de estudar as alterações em Latossolo Vermelho Distrófico causadas pelo cultivo contínuo de cana-de-açúcar, selecionaram-se três áreas (mata, cana-de-açúcar e reflorestada) adjacentes, no município de Guariba (SP). Em cada área, foram coletadas, aleatoriamente, quatro amostras, nas camadas de 0,0-0,10 m e 0,10-0,20 m. Foram avaliados os atributos químicos pH, matéria orgânica (MO), fósforo (P), potássio (K), cálcio (Ca), magnésio (Mg), alumínio (Al) e acidez potencial (H+Al), e calculados os valores de soma de bases (SB), capacidade de troca de cátions (CTC), saturação por alumínio (m%) e saturação por bases (V%). As análises de agrupamentos e componentes principais permitiram identificar a formação de três grupos, formados por mata nativa, área reflorestada e área com cana-de-açúcar. Os resultados indicam que o uso intensivo do solo alterou os seus atributos químicos. As técnicas de análises multivariadas mostraram que os principais atributos relacionados com os ambientes foram: na mata nativa, a MO, H+Al, m% e Al; na área com cana-de-açúcar, Mg, Ca, V%, SB e CTC. Enquanto que o ambiente reflorestado ficou entre os ambientes mata nativa e cana-de-açúcar.Palavras-chave: Mata nativa; cana-de-açúcar; área reflorestada. AbstractChemical properties of an oxisol under different management practices. The removal of natural vegetation for establishing an agricultural system may lead to soil imbalances according to management system used. Three adjacent areas were selected in Guariba, SP, Brazil, for the purpose of studying changes in a Latossolo Vermelho Distrófico (oxisol) caused by continuous cropping of sugarcane. In each area, four samples were collected in the 0.0-0.10 m and 0.10-0.20 m soil layers. The following chemical properties were evaluated: pH, organic matter (OM), phosphorus (P), potassium (K), calcium (Ca), magnesium (Mg), aluminum (Al), potential acidity (H+Al), and aluminum saturation (m%); and the values of the sum of bases (SB), cation exchange capacity (CEC), and base saturation (V%). Cluster analyses and principal components allowed identification the formation of three groups, made up of native forest, reforested area, and the area planted to sugarcane. Results indicate that intensive use of the soil altered its chemical properties. Multivariate analysis techniques showed that the main properties related to the environment in the native forest area were organic matter, potential acidity, aluminum saturation, and aluminum. In the sugarcane area the properties were Mg, Ca, V%, BS, SB, and CEC. The reforested area was in an intermediate position between the native forest and sugarcane environments.Keywords: Native forest; sugarcane; reforested area.

The role of active fractions of soil organic matter in physical and chemical fertility of Ferrosols

Soil Research ◽  
1998 ◽  
Vol 36 (5) ◽  
pp. 809 ◽  
Author(s):  
M. J. Bell ◽  
P. W. Moody ◽  
R. D. Connolly ◽  
B. J. Bridge
Keyword(s):  
Organic Matter ◽  
Soil Organic Matter ◽  
Management Practices ◽  
Chemical Properties ◽  
Aggregate Stability ◽  
Infiltration Rate ◽  
Exchange Capacity ◽  
Organic C ◽  
Wide Range ◽  
Physical And Chemical

The relationships between fractions of soil organic carbon (C) oxidised by varying strengths of potassium permanganate (KMnO4) and important soil physical and chemical properties were investigated for Queensland Ferrosols. These soils spanned a wide range of clay contents (31-83%), pH values (4·4-7·9; 1 : 5 water), and total C contents (12· 1-111 g/kg). Carbon fractions were derived by oxidation with 33 mM (C1), 167 mM (C2), and 333 mM (C3) KMnO4, while organic C and total C were determined by Heanes wet oxidation and combustion, respectively. Aggregate stability was determined by wet sieving soil from the surface crust after 30 min of high intensity (100 mm/h), simulated rainfall on disturbed samples in the laboratory. The proportion of aggregates <0·125 mm (P125) was used as the stability indicator because of the high correlation between this size class and the final rainfall infiltration rate (r2 = 0qa86, n = 42). The soil organic C fraction most closely correlated with P125 was C1 (r2 = 0·79, n = 42). This fraction was also highly correlated with final, steady-state infiltration rates in field situations where there were no subsurface constraints to infiltration (r2 = 0·74, n = 30). Multiple linear regression techniques were used to identify the soil properties determining effective cation exchange capacity (ECEC, n = 89). Most variation in ECEC (R2 = 0 ·72) was accounted for by a combination of C1 (P < 0·0001) and pH (P < 0·0001). These results confirm the very important role played by the most labile (easily oxidised) fraction of soil organic matter (C1) in key components of the chemical and physical fertility of Ferrosols. Management practices which maintain adequate C1 concentrations are essential for sustainable cropping on these soils.

scholarly journals Soil chemical properties in vineyard areas in the southern region of the state of Santa Catarina, Brazil

2021 ◽  
Vol 56 ◽  
Author(s):  
Samya Uchôa Bordallo ◽  
Alcenir Claudio Bueno ◽  
Guilherme Wilbert Ferreira ◽  
Emilio Dela Bruna ◽  
Izabela Sgrott Serpa ◽  
...  
Keyword(s):  
Chemical Properties ◽  
Exchange Capacity ◽  
The State ◽  
Southern Region ◽  
Base Saturation ◽  
Soil Chemical Properties ◽  
Native Forest ◽  
Santa Catarina ◽  
Soil Layers ◽  
Exchangeable Al

Abstract The objective of this work was to evaluate changes in the soil chemical properties and the critical environmental limit for phosphorus (CEL-P) in vineyards, in the southern region of the state of Santa Catarina, Brazil. Soil samples were collected at 0-5, 5-10, 10-20, and 20-40 cm soil depths, in vineyards aged 22, 36, and 60 years, and in the area of an adjacent native forest. The following parameters were analyzed: granulometry, pH in water, and exchangeable Al levels, to obtain potential acidity and Al saturation; and available levels of P and K, and exchangeable levels of Ca and Mg, to determine base saturation, cation exchange capacity; and soil organic matter (SOM). In comparison with the forest soil, the vineyard soils showed increased pH values, P, K, Ca, Mg, Cu, Zn, and SOM levels, and base saturation, as well reduced Al saturation, with more accentuated effects in areas with the longest cultivation time. The vineyards show changes in soil chemical properties with time and P levels above the CEL-P, at least in one of the soil layers.

scholarly journals Soil Chemical attributes under different management systems in Cerrado-Amazon ecotone

2021 ◽  
Vol 10 (7) ◽  
pp. e36210716045
Author(s):  
Amanda da Silva Reis ◽  
Rubson da Costa Leite ◽  
Guilherme Octávio de Sousa Soares ◽  
José Lucas de Sousa Soares ◽  
Flavia Barreira Gonçalves ◽  
...  
Keyword(s):  
Soil Chemistry ◽  
Management Practices ◽  
Secondary Forest ◽  
Principal Component ◽  
Exchange Capacity ◽  
Management Systems ◽  
Native Forest ◽  
Aluminum Saturation ◽  
Chemical Attributes ◽  
System 1

The Cerrado-Amazonas ecotone occupies 4.85% of the Brazilian territory, with almost 60% of its area deforested. Inadequate soil management practices cause changes in the physical, chemical and biological soil attributes. This study aimed to characterize soil chemistry in different management systems, identifying its efficiency. Ten areas were divided into two soil classes (Ultisol and Entisol               quartzipsamment), each comprising a management system (1 - silvopastoral with 30% shade (SP30), 2 - silvopastoral with 60% shade (SP60), 3 - secondary forest, 4 - native forest, 5 – pasture conventional (CP)). The samples were collected at depths of 0-10, 10-20 and 20-40 cm. The chemical attributes of the soil analyzed were pH, P, K +, Ca2 +, Mg2 +, H + Al3 +, Al3 +, sum of bases (SB), effective cation exchange capacity (CEC), CEC at pH 7, saturation base (V%) and aluminum saturation (m%). The data were submitted to principal component analysis and analysis of variance and Tukey's test (p <0.05). There were minor changes in the attributes analyzed in the Entisol management systems, comparing the other systems with the reference system (native forest); however, SP30 was more suitable, as it increased the pH and the values of essential cations in the soil. In Ultisol, the SP60 and CP systems showed higher averages in the studied attributes, it is inferred that these systems have similar efficiency in land use, positioning them as the best systems studied in this soil class.

scholarly journals Effect of three different agronomic conditions on biochemical profile and diversity in the rhizosphere of banana plantations infected with Fusarium oxysporum Race 1

2021 ◽  
Vol 27 (2) ◽  
Author(s):  
Katherine Sánchez-Zúñiga ◽  
◽  
Ana Tapia-Fernández ◽  
William Eduardo Rivera-Méndez ◽  
◽  
...  
Keyword(s):  
Microbial Communities ◽  
Management Practices ◽  
Soil Health ◽  
Chemical Properties ◽  
Principal Component ◽  
Exchange Capacity ◽  
High Fertility ◽  
Fertility Level ◽  
Biochemical Profile ◽  
Agronomic Conditions

Soil microorganisms play an important role as a link in the transfer of nutrients from the rhizosphere. The physical and chemical properties of soil, the metabolic profiles of microbial communities and different crop management practices can enhance our understanding of hizospheric interactions. This study aimed to establish differences in microbial communities associated with banana crops and the biochemical profile in farms under different agronomic conditions. Seven farms with different levels of intervention, management, and fusariosis severity were analyzed. The biochemical profile of the microbial community was determined using EcoPlates and the main substrates consumed by the microbial communities were identified through multivariate principal component analysis (PCA). Seven microorganisms were selected as indicators of nutrient cycles, pathogenicity and soil health. Also, soil chemical indicators were determined through a complete mineral analysis. For the physiological profile of soil microbial populations, it was observed that farms with the same management tend to be metabolically very similar. In the PCA, two principal components explained 90 % of the variance in the data. It was also determined that the genus Bacillus is predominant in all farms and that farm 4 (medium intervention) presented the most favorable values in all factors analyzed. The effective cation exchange capacity values are highlighted in the chemical analyses, which determined that all farms have a high fertility level. The metabolic profile, diversity and richness of each of the different farms were affected by the type of agronomic management used.

scholarly journals Physical properties and particle-size fractions of soil organic matter in crop-livestock integration

2012 ◽  
Vol 36 (4) ◽  
pp. 1299-1310 ◽  
Author(s):  
Carolina Tirloni ◽  
Antonio Carlos Tadeu Vitorino ◽  
Anderson Cristian Bergamin ◽  
Luiz Carlos Ferreira de Souza
Keyword(s):  
Organic Matter ◽  
Soil Quality ◽  
Crop Rotation ◽  
Cover Crops ◽  
Chemical Properties ◽  
Environmental Stability ◽  
Native Forest ◽  
Physical And Chemical Properties ◽  
Physical And Chemical ◽  
And Chemical Properties

Crop-livestock integration represents an interesting alternative of soil management, especially in regions where the maintenance of cover crops in no-tillage systems is difficult. The objective of this study was to evaluate soil physical and chemical properties, based on the hypothesis that a well-managed crop-livestock integration system improves the soil quality and stabilizes the system. The experiment was set up in a completely randomized design, with five replications. The treatments were arranged in a 6 x 4 factorial design, to assess five crop rotation systems in crop-livestock integration, and native forest as reference of soil undisturbed by agriculture, in four layers (0.0-0.05; 0.05-0.10; 0.10-0.15 and 0.15-0.20 m). The crop rotation systems in crop-livestock integration promoted changes in soil physical and chemical properties and the effects of the different systems were mainly detected in the surface layer. The crops in integrated crop-livestock systems allowed the maintenance of soil carbon at levels equal to those of the native forest, proving the efficiency of these systems in terms of soil conservation. The systems influenced the environmental stability positively; the soil quality indicator mineral-associated organic matter was best related to aggregate stability.

Changes in the properties of Fijian Oxisols over 30 years of sugarcane cultivation

Soil Research ◽  
2016 ◽  
Vol 54 (4) ◽  
pp. 418 ◽  
Author(s):  
R. J. Morrison ◽  
J. S. Gawander
Keyword(s):  
Organic Matter ◽  
Organic Carbon ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Total Production ◽  
Land Preparation ◽  
Soil Mixing ◽  
Phosphate Retention ◽  
Sugarcane Productivity ◽  
Highly Weathered Soils

Sugarcane production plateaued in Fiji at ~4 million tonnes annually (average ~55 t/ha) during the latter part of the 1980s but, in recent years, despite the continuing release of high yielding varieties, the total production has decreased to under 3 million tonnes (average ~45 t/ha). This study was initiated to study the changes in the properties of Oxisols following sugarcane cultivation to ascertain whether yield declines were due to degradation of soil biophysical and chemical properties. The study lasted from 1978 (when the soils were first cleared for agriculture) to 2009. Soil (0–15, 30–40 and 70–80 cm) properties including pH, organic carbon, cation exchange capacity, water retention, bulk density, phosphate retention and exchangeable bases were monitored. The observed topsoil changes could generally be related to changes in organic matter and associated ion exchange properties. The major changes occurred in the first three years after clearing, but some changes continued for many years. Subsoil samples (30–40 cm) showed an increase in organic carbon after cane cultivation, probably due to soil mixing during land preparation, organic matter movement during cropping and decay of sugarcane roots. At 70–80 cm, small but significant increases in organic carbon were observed along with small decreases in pH. Overall, these changes indicate that careful management of topsoils is essential for maintaining soil fertility and hence sugarcane productivity on these highly weathered soils.

scholarly journals Impact of Cement Dust on Physical and Chemical Nutrients Properties of Forest Topsoil

2021 ◽  
Vol 25 (5) ◽  
pp. 695-700
Author(s):  
A.P. Adebiyi ◽  
H.O. Adigun ◽  
K.J. Lawal ◽  
K.D. Salami ◽  
V.A.L. Adekunle ◽  
...  
Keyword(s):  
Organic Matter ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Cement Dust ◽  
Sodium Calcium ◽  
Close Proximity ◽  
Calcium Magnesium ◽  
Magnesium Cation ◽  
Physical And Chemical ◽  
Nitrogen Phosphorus

: The study examined the impact of Cement dust on physical and chemical nutrients properties of forest topsoil in close proximity to a major private cement industry in Obajana, Kogi State, Nigeria using standard methods by collecting Topsoil samples for physical and chemical properties analyses which are particle size, moisture content, pH, carbon, nitrogen,phosphorus, potassium, sodium, calcium, magnesium, cation exchange capacity and organic matter.Data revealed a strong influence of the particulate pollutants on the forest topsoil in close proximity to the Cement factory. It was observed that the soil properties; moisture content and soil pH varied at distances away from the factory. The result showed that the Cement dust particles entering the soil increased the pH of the soil, it more alkaline. The highest pH (6.03) was observed from hundred and fifty meters sample indicating the highest particulate pollution. There were also variations in the other soil nutrient properties; carbon, nitrogen, phosphorus, potassium, sodium, calcium, magnesium, cation exchange capacity and organic matter arising from the effect of cement dust. High organic matter content was recorded in the location samples compared with the control sample. This is attributed to the addition of cement dust to the soils, resulting in improved organic-matter cycling and plant growth. The result also showed that the chemical properties; organic carbon (OC), organic matter (OM), phosphorus (P), potassium (K), sodium (Na), calcium (Ca) and magnesium (Mg) are significantly higher in the study areas than the control. The study therefore concludes that the emission of cement dust on the forest stands over the years was found to have significantly affected the topsoil properties.

scholarly journals Physico-chemical characteristics of the seasonally flooded soils of Bangladesh and their management implications

1970 ◽  
Vol 20 (2) ◽  
pp. 173-182
Author(s):  
KF Akhter ◽  
ZH Khan ◽  
MS Hussain ◽  
AR Mazumder
Keyword(s):  
Organic Matter ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Matter Content ◽  
Flooded Soils ◽  
Management Implications ◽  
Available N ◽  
Physico Chemical ◽  
Seasonally Flooded

The seasonally flooded soils of Bangladesh are unique in respect of several specific characteristics and contribute toward producing bulk of its staple food - mainly rice. Having fine texture these soils are similar to the “paddy soils” of Southeast Asian floodplains and have high production potential under proper management. Six representative soil series, viz. Arial, Debidwar, Naraibag, Jalkundi, Siddirganj and Tippera from the central region of Bangladesh have been studied to evaluate some of their intrinsic physico-chemical properties and their sustainable management requirements. These soils are slightly acidic to neutral and are negatively charged with ΔpH values ranging between –0.2 and –1.2. The organic matter content in the surface soil is relatively low that decreases steadily with depth. The cation exchange capacity (CEC) of the soils varies on the basis of their clay and organic matter contents while base saturation per cent (BSP) is high. The contents of available N, P, K and S and DTPA-extractable Fe, Mn, Cu and Zn in soils are moderate and are commensurate with the contents of colloidal fractions. These soils receive several mineral nutrients annually with the sediments deposited during the monsoon floods. The characteristics like organic matter content, particle size distribution, CEC, pH and BSP that have important management implications have been discussed. Key words: Seasonally flooded soils; Physical and chemical attributes; Management implications DOI: http://dx.doi.org/10.3329/dujbs.v20i2.8978 DUJBS 2011; 20(2): 173-182

scholarly journals Characterization and Classification of Major Mango-growing Soils in Arid Part of Ananthapuramu District, Andhra Pradesh, India

Agropedology ◽  
2019 ◽  
Vol 30 (2) ◽  
Author(s):  
R. Srinivasan ◽  
◽  
R. Vasundhara ◽  
M. Lalitha ◽  
B. Kalaiselvi ◽  
...  
Keyword(s):  
Management Practices ◽  
Chemical Properties ◽  
Clay Content ◽  
Granite Gneiss ◽  
Nutrient Status ◽  
Exchange Capacity ◽  
Parent Material ◽  
Organic Carbon Content ◽  
High Base ◽  
Physical And Chemical

Four typical pedons representing major mango growing soils, developed from granite gneiss parent material were studied for their morphological, physical and chemical properties. The soils were moderately shallow (50-75 cm) to very deep (>150 cm) in depth, loamy sand to sandy clay loam in texture, sub-angular blocky in structure, reddish brown to dark red in colour, slightly acidic to moderately alkaline in reaction, non-saline, very low to high in organic carbon content (0.09 to 1.29%), low AWC (3.36 to 7.80%), low to medium in cation exchange capacity (2.90 to 19.36 cmol (p+) kg-1) and high base saturation (78 to 98%). The soils also had high amounts of coarse fragments in P1 and P2 and high clay content in P4 and P2. Among the exchangeable cations, calcium was found to be high in most of the soils, followed by magnesium, sodium, and potassium. Based on the soil characteristics, the mango growing soils were classified as Typic Haplargids and Typic Paleargids in subgroup level. Varying soil and site characters i.e., poor rainfall, shallow soil depths, excess gravel contents, low AWC, poor nutrient status and severe soil erosion are limiting the growth and development of mango plantation. Developing site-specific soils based suitable management practices can improve the productivity of mango crops.

Effect of Tillage and Cover Crop on Fluometuron Adsorption and Degradation under Controlled Conditions

Weed Science ◽  
1994 ◽  
Vol 42 (4) ◽  
pp. 629-634 ◽  
Author(s):  
Blake A. Brown ◽  
Robert M. Hayes ◽  
Donald D. Tyler ◽  
Thomas C. Mueller
Keyword(s):  
Organic Matter ◽  
Soil Organic Matter ◽  
Soil Ph ◽  
Cover Crop ◽  
Soil Depth ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Matter Content ◽  
No Till

Fluometuron adsorption and degradation were determined in soil collected at three depths from no-till + no cover, conventional-till + no cover, no-till + vetch cover, and conventional-till + vetch cover in continuous cotton. These combinations of tillage + cover crop + soil depth imparted a range of organic matter and pH to the soil. Soil organic matter and pH ranged from 0.9 to 2.5% and from 4.7 to 6.5, respectively. Fluometuron adsorption was affected by soil depth, tillage, and cover crop. In surface soils (0 to 4 cm), fluometuron adsorption was greater in no-till + vetch plots than in conventional-tilled + no cover plots. Soil adsorption of fluometuron was positively correlated with organic matter content and cation exchange capacity. Fluometuron degradation was not affected by adsorption, and degradation empirically fit a first-order model. Soil organic matter content had no apparent effect on fluometuron degradation rate. Fluometuron degradation was more rapid at soil pH > 6 than at pH ≤ 5, indicating a potential shift in microbial activity or population due to lower soil pH. Fluometuron half-life ranged from 49 to 90 d. These data indicate that tillage and cover crop may affect soil dissipation of fluometuron by altering soil physical and chemical properties that affect fluometuron degrading microorganisms or bioavailability.

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