scholarly journals Relationship between soil fertility and plantain nutrition in Cundinamarca (Colombia) with the incidence of two bacterial diseases

2020 ◽  
Vol 14 (1) ◽  
Author(s):  
Luis Gabriel Bautista-Montealegre ◽  
Sebastián David García-Guzmán ◽  
Martha Marina Bolaños-Benavides
Keyword(s):  
Large Scale ◽  
Descriptive Analysis ◽  
Management Strategies ◽  
Chemical Properties ◽  
Distribution Patterns ◽  
Exchange Capacity ◽  
Low Fertility ◽  
La Palma ◽  
Chemical Properties Of Soils ◽  
Foliar Concentration

The bacteriosis and moko of plantain are ones of the most important phytosanitary problems in the production of musaceae in Colombia. To contribute to the management of these diseases in the department of Cundinamarca, soils and foliar tissues were analyzed, as well as the symptoms of the diseases in 149 farms of producers in the municipalities of Chaguani, La Palma, La Vega, and Viota (Cundinamarca). A descriptive analysis of the chemical properties of soils and foliar concentration of nutrients was carried out; the Student-Welch t-test was applied (P<0.05); the distribution patterns of the diseases were represented cartographically. According to the results obtained, the sampled soils are not saline, they have extreme to strong acidity, low effective cation exchange capacity and low fertility; meanwhile plants show a deficit of elements such as nitrogen, phosphorus, sulfur, copper, zinc, and boron. Considering the total number of farms evaluated, the incidence of bacteriosis and moko disease was reported in 63 and 14% at the departmental level, respectively. A higher concentration of sulfur and zinc was observed in farm soils free of both diseases. Finally, plants reported as free of bacteriosis showed a higher concentration of potassium and lower concentrations of calcium and manganese; while plants reported as free of moko disease showed higher concentrations of nitrogen, sodium, and copper, and a lower concentration of calcium. The results obtained contribute to the planning of large-scale management strategies, in order to reduce the risk of dissemination of diseases of economic importance for plantain crop.

Physical and chemical characteristics of duplex soils and their distribution in the south-west of Western Australia

1992 ◽  
Vol 32 (7) ◽  
pp. 827 ◽  
Author(s):  
D Tennant ◽  
G Scholz ◽  
J Dixon ◽  
B Purdie
Keyword(s):  
Western Australia ◽  
Management Strategies ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Low Fertility ◽  
Low Permeability ◽  
The South ◽  
Sand Surface ◽  
South West ◽  
Physical And Chemical

Duplex soils are widespread in Western Australia and occupy about 60% of the south-west agricultural area. The physical and chemical properties of these soils reflect their origin as erosional surfaces of old laterite profiles and the predominance of underlying, quartz-rich, granitic materials. The resulting combination of high contents of quartz sand, kaolin clay, and iron and aluminium oxides has important consequences on water-holding capacity, fertility, nutrient leaching, phosphate fixation, anion and cation exchange capacity, and buffering capacity. These soils are generally held to have a number of physical and chemical problems. Among these, low fertility and low permeability of the clay B horizon have greatest effect. While data on the chemical properties of these soils are limited, significant data sets on the physical properties of duplex soils are available from several studies of catchment hydrology. These studies reflect concern with runoff, waterlogging, and the development of secondary salinisation. Depth to clay varies from 5 to >100 cm. The shallower depths (10-40 cm) predominate and, in medium and high rainfall areas, combine with low permeability in the clay to result in widespread waterlogging. Commonly, the sand surface can be hardsetting and can have high strength from structural decline, from the presence of cementing agents, and from traffic effects. Sodicity is widespread and has effects on hardsetting in the A horizon and on permeability of the B horizon. Management strategies are available to treat some of these problems, but generally, much has yet to be done to develop sustainable agricultural systems on these soils.

scholarly journals Effect of termite activity on soil under different land management strategies

2017 ◽  
Vol 38 (1) ◽  
pp. 143
Author(s):  
Liane Barreto Alves Pinheiro ◽  
Rodrigo Camara ◽  
Marcos Gervasio Pereira ◽  
Eduardo Lima ◽  
Maria Elizabeth Fernandes Correia ◽  
...  
Keyword(s):  
Organic Carbon ◽  
Management Strategies ◽  
Chemical Properties ◽  
Clay Content ◽  
Exchange Capacity ◽  
Termite Mounds ◽  
Eucalyptus Plantation ◽  
Exchangeable Acidity ◽  
Calcium And Magnesium ◽  
Surrounding Soil

Mound-building termites are important agents of soil bioperturbation, but these species have not been extensively studied thus far. The present study aimed to evaluate the soil particle-size and the chemical attributes of termite mounds and the surrounding soil under different land use strategies. A one-hectare plot was defined for an unmanaged degraded pasture, planted pasture, and for a eucalyptus Corymbia citriodora plantation. In each plot, the top, center, and base sections of five Cornitermes cumulans mounds, and the surrounding soil at the depths of 0-5; 5-10; 10-20 cm, were sampled in the Pinheiral, Rio de Janeiro state. In the three areas, the center of the mounds contained higher clay content, organic carbon, phosphorous, calcium and magnesium, total bases, and cation exchangeable capacity, when compared to the top, base, and the surrounding soils. However, the center had lower values of exchangeable acidity and potassium, of the three areas. In the eucalyptus plantation, the values of pH, total bases, calcium, and magnesium were lower, whereas aluminum, exchangeable acidity, sodium, and cation exchange capacity were higher both in the mounds and in the surrounding soil, in relation to the pastures. There were no differences among the three areas in terms of organic carbon, potassium, phosphorous, and total bases, in the mounds and adjacent soil. Thus, the termite activity altered the clay content and most of the soil chemical properties in all of the studied areas, but only for the center of the mounds. However, the effect of these organisms was different in the eucalyptus plantation in relation to the pasture areas.

Long-Term Effects of Fertilizers and Manure on Soil and Leaves of Cotton in Nigeria

1969 ◽  
Vol 5 (3) ◽  
pp. 241-247 ◽  
Author(s):  
B. W. Bache ◽  
R. G. Heathcote
Keyword(s):  
Potassium Chloride ◽  
Ammonium Sulphate ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Long Term Effects ◽  
Single Superphosphate ◽  
Exchangeable Ca ◽  
Chemical Properties Of Soils ◽  
Sudan Savanna ◽  
A Site

SummaryOn a site in the Sudan Savanna, chemical properties of soils (except for phosphate) and the composition of cotton leaves were determined after fifteen annual treatments including dung, ammonium sulphate, single superphosphate and potassium chloride, in all combinations of three levels. In the soils dung increased C, N, cation exchange capacity, exchangeable Ca and Mg and pH, and decreased soluble Al and Mn; ammonium sulphate decreased pH, increased soluble Al and Mn, and decreased exchangeable Ca and Mg; potassium chloride had no obvious effects. In the plants dung increased P and reduced Mn; ammonium sulphate reduced Ca and Mg, and increased Mn; superphosphate increased P, Ca and Mg, and reduced K; potassium chloride increased K slightly. The most important results were the ability of ammonium sulphate to acidify the soil, as shown by soil properties and reflected in tissue composition, and the ability of dung to ameliorate these effects. Reduction of crop yield in the presence of adequate nutrient supply seems to have been due to excessive soil acidity.

scholarly journals Does thermal carbonization (Biochar) of organic material increase more merits for their amendments of sandy soil?

2014 ◽  
Vol 6 (1) ◽  
pp. 535-558 ◽  
Author(s):  
Y. Wu ◽  
G. Xu ◽  
J. N. Sun ◽  
H. B. Shao
Keyword(s):  
Soil Ph ◽  
Saline Soil ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Low Fertility ◽  
Available P ◽  
Available Phosphorus ◽  
Furfural Residue ◽  
Leaching Solution ◽  
Physical And Chemical

Abstract. Organic materials (e.g. furfural residue) are generally believed to improve the physical and chemical properties of the soils with low fertility. Recently, biochar have been received more attention as a possible measure to improve the carbon balance and improve soil quality in some degraded soils. However, little is known about their different amelioration of a sandy saline soil. In this study, 56d incubation experiment was conducted to evaluate the influence of furfural and its biochar on the properties of saline soil. The results showed that both furfural and biochar greatly reduced pH, increased soil organic carbon (SOC) content and cation exchange capacity (CEC), and enhanced the available phosphorus (P) in the soil. Furfural is more efficient than biochar in reducing pH: 5% furfural lowered the soil pH by 0.5–0.8 (soil pH: 8.3–8.6), while 5% biochar decreased by 0.25–0.4 due to the loss of acidity in pyrolysis process. With respect to available P, 5% of the furfural addition increased available P content by 4–6 times in comparison to 2–5 times with biochar application. In reducing soil exchangeable sodium percentage (ESP), biochar is slightly superior to furfural because soil ESP reduced by 51% and 43% with 5% furfural and 5% biochar addition at the end of incubation. In addition, no significant differences were observed between furfural and biochar about their capacity to retain N, P in leaching solution and to increase CEC in soil. These facts may be caused by the relatively short incubation time. In general, furfural and biochar have different amendments depending on soil properties: furfural was more effectively to decrease pH and to increase available P, whereas biochar played a more important role in increasing SOC and reducing ESP of saline soil.

Properties of soils in the marginal upland of Sta. Rita, Samar, Philippines

2017 ◽  
pp. 1-19
Author(s):  
Kenneth Oraiz ◽  
Victor Asio
Keyword(s):  
Crop Production ◽  
Chemical Properties ◽  
The Philippines ◽  
Exchange Capacity ◽  
Ecological Problem ◽  
High Porosity ◽  
Total N ◽  
Upland Soils ◽  
Chemical Properties Of Soils ◽  
High Base

The widespread occurrence of marginal uplands is a serious agricultural and ecological problem in the Philippines. The study evaluated the morphological and physico-chemical properties of soils in the marginal upland of Sta. Rita, Samar. Three soil profiles located at different physiographic positions were examined and sampled. Findings revealed that the marginal upland soils were derived from mudstone. They were characterized by an Ap-Bt-BC horizon sequence and they were clayey with moderate to high porosity and water holding capacity values. The soils were friable in their surface horizons when moist, but plastic and sticky when wet. The soils had pH(water) values ranging from 5.20 to 6.86, indicating that soil acidity was not yet a serious problem in these soils. The soils had moderate soil organic matter contents in their surface horizons but low amounts in subsurface horizons. Total N and available P of the soils were low and a problem for crop production. However, the soils had moderate to high exchangeable bases and cation exchange capacity values. In terms of degree of soil development, the marginal upland soils was observed to be mature as reflected by their horizonation, particularly by the presence of an argillic horizon (B horizon with high clay accumulation). But they still had high base saturation, suggesting that they were not yet highly leached and thus, were classified as Typic Hapludalfs or Haplic Luvisols.

scholarly journals Chemical properties of soils treated with biological sludge from gelatin industry

2012 ◽  
Vol 36 (2) ◽  
pp. 653-660 ◽  
Author(s):  
Rita de Cássia Melo Guimarães ◽  
Mara Cristina Pessôa da Cruz ◽  
Manoel Evaristo Ferreira ◽  
Carlos Alberto Kenji Taniguchi
Keyword(s):  
Organic Matter Content ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Matter Content ◽  
P Availability ◽  
Base Content ◽  
Biological Sludge ◽  
Randomized Design ◽  
Chemical Properties Of Soils ◽  
The Impact

The impact of agro-industrial organic wastes in the environment can be reduced when used in agriculture. From the standpoint of soil fertility, residue applications can increase the organic matter content and provide nutrients for plants. This study evaluated the effect of biological sludge from gelatin industry on the chemical properties of two Ultisols (loamy sand and sandy clay) and an Oxisol (clay). The experiment lasted 120 days and was carried out in laboratory in a completely randomized design with factorial arrangement, combining the three soils and six biological sludge rates (0, 100, 200, 300, 400, and 500 m³ ha-1), with three replications. Biological sludge rates of up to 500 m³ ha-1 decreased soil acidity and increased the effective cation exchange capacity (CEC) and N, Ca, Mg, and P availability, without exceeding the tolerance limit for Na. The increase in exchangeable base content, greater than the effective CEC, indicates that the major part of cations added by the sludge remains in solution and can be lost by leaching.

scholarly journals Furfural and its biochar improve the general properties of a saline soil

Solid Earth ◽  
2014 ◽  
Vol 5 (2) ◽  
pp. 665-671 ◽  
Author(s):  
Y. Wu ◽  
G. Xu ◽  
H. B. Shao
Keyword(s):  
Soil Ph ◽  
Saline Soil ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Low Fertility ◽  
Available P ◽  
Available Phosphorus ◽  
Leaching Solution ◽  
Decreasing Ph ◽  
Physical And Chemical

Abstract. Organic materials (e.g., furfural residue) are generally believed to improve the physical and chemical properties of saline soils with low fertility. Recently, biochar has been received more attention as a possible measure to improve the carbon balance and improve soil quality in some degraded soils. However, little is known about their different amelioration of a sandy saline soil. In this study, 56 d incubation experiment was conducted to evaluate the influence of furfural and its biochar on the properties of saline soil. The results showed that both furfural and biochar greatly reduced pH, increased soil organic carbon (SOC) content and cation exchange capacity (CEC), and enhanced the available phosphorus (P) in the soil. Furfural is more efficient than biochar in reducing pH: 5% furfural lowered the soil pH by 0.5–0.8 (soil pH: 8.3–8.6), while 5% biochar decreased by 0.25–0.4 due to the loss of acidity in pyrolysis process. With respect to available P, furfural addition at a rate of 5% increased available P content by 4–6 times in comparison to 2–5 times with biochar application. In reducing soil exchangeable sodium percentage (ESP), biochar is slightly superior to furfural because soil ESP reduced by 51% and 43% with 5% furfural and 5% biochar at the end of incubation. In addition, no significant differences were observed between furfural and biochar about their capacity to retain N, P in leaching solution and to increase CEC in soil. These facts may be caused by the relatively short incubation time. In general, furfural and biochar exhibited a different effect depending on the property: furfural was more effective in decreasing pH and increasing available P, whereas biochar played a more important role in increasing SOC and reducing ESP of saline soil.

scholarly journals Effects of Management Practices on Soil Properties and Plant Nutrition in Hay Meadows in Picos de Europa

Environments ◽  
2021 ◽  
Vol 8 (5) ◽  
pp. 38
Author(s):  
Judith Álvarez ◽  
Elías Afif ◽  
Tomás E. Díaz ◽  
Laura García ◽  
Jose A. Oliveira
Keyword(s):  
Soil Properties ◽  
Management Practices ◽  
Chemical Properties ◽  
Clay Content ◽  
Exchange Capacity ◽  
Nutrient Concentrations ◽  
Mean Values ◽  
Hay Meadows ◽  
Natural Grasslands ◽  
Chemical Properties Of Soils

Fertilization and mowing affects the physico-chemical properties of soils, as well as the characteristics of the plants growing on them. Changes in the management techniques are causing semi-natural grasslands to disappear all over Europe. These grasslands host a great amount of diversity, thus their conservation is a top priority. This work studies whether the kind of management has an influence on the soil properties and the foliar content in macronutrients in 25 hay meadows located in Picos de Europa (10 in Asturias, 10 in Castilla y León and 5 in Cantabria). Soils at a 0–20 cm depth showed a high content of organic matter and a low C/N ratio. Effective cation exchange capacity was adequate for a texture, which varied from sandy clay loam to loam, with an average clay content of 17%. Mean values of foliar nutrient concentrations showed a deficiency in K. In this study, management practices were shown to affect some properties of the soils, namely pH, sand percentage and exchangeable K and Ca, to different extents. The highest values of pH and exchangeable Ca were significantly correlated with the least intensive management.

scholarly journals Physico-chemical Properties of Soil of Rangapani Tea Estate of Bangladesh

2011 ◽  
Vol 3 (3) ◽  
pp. 683-688
Author(s):  
M. N. Islam ◽  
A. F. M. Sanaullah
Keyword(s):  
Cation Exchange ◽  
Cation Exchange Capacity ◽  
Chemical Properties ◽  
Clay Content ◽  
Exchange Capacity ◽  
Soil Samples ◽  
Physico Chemical ◽  
Different Depths ◽  
Chemical Properties Of Soils ◽  
Topographic Positions

Bangladesh is one of the tea producing countries of the world. It has 163 tea estates. Rangapani is a low yielding tea estate relative to other neighboring tea estates of Chittagong district in Bangladesh. A total 54 soil samples were collected from six different hills and three topographic positions having different depths of Rnagapanni Tea-Estate. Physico-Chemical properties of soils such as active acidity, reserve acidity, cation exchange capacity and clay content of the collected soil samples were determined. The measured parameters of the soil samples were plotted and analyzed with reference to site and topography. The parameters have been found to vary with sampling sites, depths and topography. Active acidity and reserve acidity were very low, with some exceptions compared to the optimum range for tea cultivation. Sand, silt, clay and cation exchange capacity (CEC) were found in reasonable range Keywords:  Soil; Active acidity; Reserve acidity; Cation exchange capacity; Clay content. © 2011 JSR Publications. ISSN: 2070-0237 (Print); 2070-0245 (Online). All rights reserved. doi: 10.3329/jsr.v3i3.7503               J. Sci. Res. 3 (3), 683-688 (2011)

scholarly journals SPATIALITY OF SOIL CHEMICAL ATTRIBUTES IN A BANANA CULTIVATION AREA IN WEST BAHIA

2021 ◽  
Vol 34 (1) ◽  
pp. 177-188
Author(s):  
BARBEMILE DE ARAÚJO DE OLIVEIRA ◽  
LILIANE PEREIRA CAMPOS ◽  
SAMMY SIDNEY ROCHA MATIAS ◽  
TAMIRES SOARES DA SILVA ◽  
ADRIANO VENICIÚS SANTANA GUALBERTO
Keyword(s):  
Spatial Variability ◽  
Descriptive Analysis ◽  
Exchange Capacity ◽  
Soil Samples ◽  
Chemical Degradation ◽  
Low Fertility ◽  
Distribution Maps ◽  
Fruit Growing ◽  
Chemical Attributes ◽  
Irrigated Perimeter

ABSTRACT Irrigated fruit growing in the São Francisco Valley has been standing out in the Northeast region of Brazil and the incorrect management of fertilization has caused problems of physical and / or chemical degradation of the soil. The work aimed to evaluate the spatial variability of the chemical attributes of a Latossolo Vermelho-Amarelo (Oxisol) grown with banana (Musa spp). The study was carried out in the irrigated perimeter of Nupeba in Riachão das Neves / BA. In an area cultivated for 18 years with silver banana fertigated by micro sprinkling. In April 2017 simple soil samples were collected at depths of 0 -0.20 m and 0.20 -0.40 m, from an experimental grid consisting of 40 georeferenced points and spaced every 10 meters. The soil samples determined: pH (H2O); Organic carbon; Phosphorus (P); Potassium (K+); Calcium (Ca2+); Magnesium (Mg2+) and Potential acidity (H + Al) and the sum of bases (BS), cation exchange capacity (CEC) and base saturation (V%) were calculated. The results of the analyses were evaluated using descriptive statistics and the geostatistics technique. The descriptive analysis identified the normality of the data. The spatial variability was confirmed, allowing the making of maps. The analyzed area has low fertility (V <55%) and the inadequate management of soil correction and fertilization can reduce the availability of nutrients for the implanted crop, making the soil susceptible to degradation with the use of irrigation. The distribution maps allow the visualization of the area, allowing the application of inputs with varying rates, aiming at homogenizing the soil fertility.

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