scholarly journals Soil fertility status of some mango orchards in Chittagong Hill Tracts

2013 ◽  
Vol 6 (1-2) ◽  
pp. 187-197
Author(s):  
MG Kibria ◽  
MJ Ahammad ◽  
KT Osman
Keyword(s):  
Organic Matter ◽  
Soil Ph ◽  
Sandy Loam ◽  
Mangifera Indica ◽  
Chemical Properties ◽  
Available P ◽  
Total N ◽  
Physico Chemical ◽  
Soil Fertility Status ◽  
Orchard Soils

Major physico-chemical properties of mango orchard soils (Mangifera indica L.) in different sites of three hill districts, Rangamati, Khagrachari and Bandarban were evaluated. Soils were sandy loam in texture at all the sites except foot hill soil of Shapchari. Soil pH, organic matter, total N and available P varied from 4.76 to 5.58, 1.43 to 2.49 %, 0.10 to 0.16 %, 0.86 mg kg-1 to 2.69 mg kg-1 soil, respectively in surface soil of different sites of mango orchard. 1N NH4OAc extractable K+, Ca2+ and Mg2+ ranged from 0.35 to 0.82, 2.50 to 3.66 and 0.60 to 1.57 cmol kg-1 of soils. Soil pH, organic matter, total N and available P varied significantly among the slope positions within the sites. Similar results were found in case of 1N NH4OAc extractable K+, Ca2+ and Mg2+. The soils are generally poor in organic matter and nutrients. DOI: http://dx.doi.org/10.3329/cujbs.v6i1-2.17244 The Chittagong Univ. J. B. Sci.,Vol. 6(1&2):187-197, 2011

scholarly journals Physico-chemical properties of acid soils from Madhupur Tract and Northern & Eastern Piedmont Plains of Bangladesh

2021 ◽  
Vol 7 (1) ◽  
pp. 12-20
Author(s):  
Asif Ahmed Ratul ◽  
Tahsina Sharmin Hoque ◽  
Md Rafiqul Islam ◽  
Md Anamul Hoque
Keyword(s):  
Soil Ph ◽  
Crop Production ◽  
Sandy Loam ◽  
Chemical Properties ◽  
Acid Soils ◽  
Soil Samples ◽  
Soil Reaction ◽  
Total N ◽  
Organic C ◽  
Physico Chemical

Soil reaction is an important issue that adversely affects soil fertility and crop productivity. Twenty five representative soil samples from farmers’ fields of Ramchandrakura, Bishgiripar, Andharupara and Nayabil villages of Nalitabari upazila under Sherpur district (AEZ 22-Northern and Eastern Piedmont Plains) and twenty soil samples from farmers’ fields of Bakta, Nishchintopur, Boril and Kaladaho villages of Fulbaria upazila under Mymensingh district (AEZ 28-Madhupur Tract) were collected and analyzed to study the physico-chemical properties of acid soils. Among 45 samples, 13 were sandy loam, 17 were silt loam, 10 were loam, 2 were clay loam and 3 were loamy sand in texture. Soil pH was very strongly acidic to strongly acidic. The soil pH of AEZ 22 varied from 3.81 to 4.78 and that of AEZ 28 varied from 3.96 to 5.11. The organic C of Nalitabari soil varied from 0.50 to 1.35% and that of Fulbaria soils ranged from 0.50 to 1.27% showing low to medium status. The status of nutrient elements viz. N, P, K and S in most of the samples was very low or very low to medium. Total N contents of AEZ 22 varied from 0.06 to 0.14% and that of AEZ 28 varied from 0.07 to 0.16%. Available P in soils of AEZ 22 varied from 3.25 to 26.45 ppm and that in soils of AEZ 28 ranged from 2.45 to 16.62 ppm. Exchangeable K in AEZ 22 soils varied from 15.13 to 92.41 ppm and that in AEZ 28 soils varied from 16.09 to 98.41 ppm. Available S in AEZ 22 soils varied from 1.68 to 33.70 ppm and that in AEZ 28 soils from 3.95 to 27.52 ppm. Therefore, these acid soils should be amended with liming materials and fertilized with inorganic fertilizers and organic manures for successful crop production. Asian J. Med. Biol. Res. March 2021, 7(1): 12-20

The Effects of a Wildfire on Soil Chemical and Biological Properties in an Eucalyptus urophylla Forest

2013 ◽  
Vol 864-867 ◽  
pp. 2492-2497
Author(s):  
Gan Wen Lie ◽  
Long Hua Ye ◽  
Hai Yong Bao ◽  
Hong Yue Chen ◽  
Li Xue
Keyword(s):  
Organic Matter ◽  
Soil Ph ◽  
Chemical Properties ◽  
Biological Properties ◽  
Available P ◽  
Total N ◽  
Significant Difference ◽  
Bacteria And Fungi ◽  
Total P ◽  
Burned Forest

In this study, soil pH, organic matter, total N, total P, total K, alkali-hydrolyzable N, available P, available K, number of microorganism and enzyme activity were studied in a burnedE. urophyllaforest (the burned forest) and an unburned adjacentE. urophyllaforest (the control) in Dongyuan County, Guangdong Province, China. This study aims at investigating the effects of a single wildfire on soil properties of anE. urophyllaforest to provide basis for the recovery of soil fertility and management of burnedE. urophyllaforests. Significant differences were observed between the burned forest and the control in most of chemical properties. The wildfire significantly decreased the soil organic matter, total N, total P, total K, alkali-hydrolyzable N and available K by 32.8%, 33.6%, 36.8%, 35.2%, 25.0% and 28.5%, respectively. However, no significant difference was observed in soil pH and available P. The numbers of bacteria and fungi in burned forest were significant lower than those of the control, while there was no difference in actinomycetes between the two forests. The urease, phosphatase and catalase activities were statistically significant lower than those of the control. The results suggested that there were significant effects on theE. urophyllaforest 1 year after the wildfire and the recovery from the wildfire may take a long time.

scholarly journals IMPACT OF AGRO-ENVIRONMENTAL SYSTEMS ON SOIL EROSION PROCESSES AND SOIL PROPERTIES ON HILLY LANDSCAPE IN WESTERN LITHUANIA

2015 ◽  
Vol 24 (1) ◽  
pp. 60-69 ◽  
Author(s):  
Gintaras JARAŠIŪNAS ◽  
Irena KINDERIENĖ
Keyword(s):  
Soil Erosion ◽  
Soil Properties ◽  
Soil Ph ◽  
Soil Texture ◽  
Sandy Loam ◽  
Chemical Properties ◽  
Available Phosphorus ◽  
Erosion Processes ◽  
Physico Chemical ◽  
The Impact

The objective of this study was to evaluate the impact of different land use systems on soil erosion rates, surface evolution processes and physico-chemical properties on a moraine hilly topography in Lithuania. The soil of the experimental site is Bathihypogleyi – Eutric Albeluvisols (abe–gld–w) whose texture is a sandy loam. After a 27-year use of different land conservation systems, three critical slope segments (slightly eroded, active erosion and accumulation) were formed. Soil physical properties of the soil texture and particle sizes distribution were examined. Chemical properties analysed for were soil ph, available phosphorus (P) and potassium (K), soil organic carbon (SOC) and total nitrogen (N). We estimated the variation in thickness of the soil Ap horizon and soil physico-chemical properties prone to a sustained erosion process. During the study period (2010–2012) water erosion occurred under the grain– grass and grass–grain crop rotations, at rates of 1.38 and 0.11 m3 ha–1 yr–1, respectively. Soil exhumed due to erosion from elevated positions accumulated in the slope bottom. As a result, topographic transfiguration of hills and changes in soil properties occurred. However, the accumulation segments of slopes had significantly higher silt/clay ratios and SOC content. In the active erosion segments a lighter soil texture and lower soil ph were recorded. Only long-term grassland completely stopped soil erosion effects; therefore geomorphologic change and degradation of hills was estimated there as minimal.

scholarly journals Changes in physico-chemical properties of paddy soil due to water and fertilizer management

2020 ◽  
Vol 5 (2) ◽  
pp. 65-71
Author(s):  
Israt Jahan ◽  
AKM Abul Ahsan ◽  
MMR Jahangir ◽  
Mahmud Hossain ◽  
Md Anwarul Abedin
Keyword(s):  
Organic Matter ◽  
Soil Properties ◽  
Bulk Density ◽  
Total Nitrogen ◽  
Soil Ph ◽  
Crop Production ◽  
Soil Health ◽  
Chemical Properties ◽  
Soil Samples ◽  
Physico Chemical

Soil physico-chemical properties are an important phenomenon for sustainable crop production and maintenance of optimum soil health. Hence, a laboratory measurement was conducted with soil samples of three years long experimental field of the Department of Soil Science, Bangladesh Agricultural University, Mymensingh to assess the changes in five selected soil physico-chemical properties viz. soil texture, bulk density, soil pH, total nitrogen and organic matter. The experiment was laid out in a split plot design with two water regimes (continuous flooding and alternate wetting & drying) in the main plots and five fertilizer treatments (N0 - control, N1- 140 kg N/ha as PU, N2- 104 kg N/ha as USG (2× 1.8 g/ 4 hills), N3 - 5 t CD + PU @ 140 kg N /ha on IPNS basis and N4- 5 t CD + USG (2× 1.8 g/ 4 hills @ 104 kg N/ha)) in the subplots under rice-rice cropping pattern with three replications. After three years, soil samples were collected at 0-5 and 5-10 cm soil depths for measuring bulk density and at 0-10 cm depth for other soil properties and analyzed. Results found that % sand, % silt, % clay, bulk density and soil pH was not changed significantly compared to initial status. Percentage of total nitrogen and organic matter was significantly affected by irrigation and fertilization. Total nitrogen (%) was higher in AWD whereas organic matter (%) was higher in CF practice. The highest total nitrogen (%) and organic matter (%) was found in N4 treatment in which USG was applied in combination with cowdung as organic manure. It can be suggested that N4 treatment was formed good combination for sustaining chemical properties of soil. Further long- term experimentation will be needed to know the changes in soil properties for sustainable crop production and improving soil health. Asian Australas. J. Biosci. Biotechnol. 2020, 5 (2), 65-71

scholarly journals Soil Physico-chemical Properties Changes under Different Crops in Ado Ekiti, Nigeria

2018 ◽  
pp. 1-15 ◽  
Author(s):  
G. O. Awe ◽  
O. O. Nurudeen ◽  
S. O. Omotoso ◽  
A. A. Amiola ◽  
D. Ojeniyi ◽  
...  
Keyword(s):  
Soil Ph ◽  
Cover Crops ◽  
Sandy Loam ◽  
Cropping Systems ◽  
Chemical Properties ◽  
Agricultural Practices ◽  
Phosphate Fertilizer ◽  
Soil Chemical Properties ◽  
Physico Chemical ◽  
Classical Statistics

The sustainable soil management necessary to maintain soil quality depends on the understanding of how the soil responds to agricultural practices over time. This paper reports the changes in physicochemical properties that resulted from different cropping systems on a soil in Ado Ekiti, Nigeria. Soil samples were collected from sole maize plot (1.0 ha), sole cowpea plot (1.0ha) and cassava/maize intercrop plot (0.6ha) on a land that was previously under fallow. The sand, silt and clay contents of the soil and some selected chemical parameters varied considerably within the study area (different cropping zones). The soil was generally sandy loam and was found to vary from slightly acidic to slightly alkaline and generally low in Soil Organic Matter (SOM) and Available P (Av. P) with no salinity problem. High magnitude of variability was observed for Electrical Conductivity (EC), Av. P and SOM while pH had the least magnitude. A geostatistical evaluation of the soil chemical properties showed moderate to strong spatial dependence. The geospatial maps clearly revealed the heterogeneity of the soil chemical properties across the field. Both classical statistics and geo-statistical analyses of the soil of the area provided a better understanding of the spatial variability of soil chemical properties and the influence that such could have on crop performance. The results indicated that the soil pH is slightly acidic and contained low amounts of both SOM and Av. P. It is suggested that planting of cover crops, minimum tillage and controlled application of phosphate fertilizer should be done so as to increase the SOM, improve Av. P and maintain the soil pH. Further studies should be conducted to include other soil chemical properties such that robust site specific management programme could be effected.

scholarly journals Physico-chemical characterization of some selected soil series of Mymensingh and Jamalpur districts of Bangladesh

2016 ◽  
Vol 13 (2) ◽  
pp. 197-206
Author(s):  
PR Sheel ◽  
MAH Chowdhury ◽  
M Ali ◽  
MA Mahamud
Keyword(s):  
Sandy Loam ◽  
Chemical Properties ◽  
Chemical Characterization ◽  
Agricultural Practices ◽  
Soil Series ◽  
Total N ◽  
Positive Correlation ◽  
Physico Chemical ◽  
Very High

The soil physico-chemical properties have been disturbed due to long continued intensive agricultural practices. Under this situation we are approaching rapidly to a very strong future challenge in sustaining the quality of our soil. This study was conducted to evaluate the physico-chemical properties of the selected soil series. The area covered Mymensingh and Jamalpur districts of Bangladesh. Soil samples were collected randomly from different profiles of Lokdeo, Tarakanda, Silmondi and Melandah soil series during March-May, 2014 and analysed. All soils were acidic and textural classes were sandy loam, silt loam, loam, and clay loam. Organic matter and total N contents low to very low. Available S content in the upper layers of most soils were medium to optimum and in the deeper layer low to medium. The exchangeable K, Ca and Na contents were also low. The upper layers of all the locations contained higher amounts of available Zn. The available Cu and Fe contents of most soils were very high. The soils of all locations contained very high amount of available Mn except the deeper layers (45-75 cm) of Melandah which contained optimum amount of available Mn. Soil pH showed negative correlation with total N and available S. Total N showed positive correlation with soil OM, available Cu and available S. There was positive correlation between available S and available Mn.J. Bangladesh Agril. Univ. 13(2): 197-206, December 2015

scholarly journals Intensive Vegetable Production Degrades Volcanic Ash Soil in Cabintan, Ormoc City, Philippines

2020 ◽  
Vol 14 (1) ◽  
pp. 36-53
Author(s):  
Frances Mae Pizon ◽  
◽  
Anabella B. Tulin ◽  
Keyword(s):  
Organic Matter ◽  
Soil Ph ◽  
Volcanic Ash ◽  
Chemical Properties ◽  
Soil Management ◽  
Available Phosphorus ◽  
Vegetable Production ◽  
Exchangeable Bases ◽  
Physico Chemical ◽  
Volcanic Ash Soil

Long-term intensive cultivation leads to soil-related problems. This study was conducted to know the changes in physico-chemical properties of volcanic ash soil (Andisol) in Barangay Cabintan, Ormoc City, Leyte after ten years of intensive vegetable production. Five sampling sites were selected, representing fallow and intensively cultivated areas. The soils were collected and analyzed for particle size analysis (PSA), bulk density (Db), soil pH, organic matter (OM), nitrogen (N), available phosphorus (P) and exchangeable bases potassium (K), magnesium (Mg), calcium (Ca), and sodium (Na). The findings of the current study were compared to the results reported by the ACIAR project ten years ago. The results revealed that the soil physico-chemical properties of Andisol changed within ten years. There were significant differences in soil physicochemical properties of Andisol across sites and depths as influenced by the two types of soil management over ten years. Soil management practices influenced the nutrient supplying capacity and the physico-chemical properties of the soil. Soil texture did not vary except for sites C and E (intensively cultivated areas). The bulk density remained low while the soil pH, soil organic matter, nitrogen, and exchangeable bases decreased. However, the available phosphorus increased under intensive vegetable production. The overall results highlighted the need to employ the appropriate soil management, specifically fertilizer application. An accurate and exact combination of organic and inorganic fertilizers is highly recommended in the area to obtain the desired vegetable yield.

scholarly journals Edaphic macrofauna and soil physicochemical properties, in smallholder coffee farms

2021 ◽  
Vol 38 (4) ◽  
pp. 934-950
Author(s):  
Eli Morales ◽  
Segundo Chávez ◽  
Elder Chichipe ◽  
Manuel Oliva ◽  
Lenin Quiñones
Keyword(s):  
Organic Matter ◽  
Soil Ph ◽  
Chemical Properties ◽  
Shannon Index ◽  
Small Scale ◽  
Lower Altitude ◽  
Physico Chemical ◽  
Soil Indicator ◽  
Coffee Farmers ◽  
Time Of Year

Edaphic macrofauna is a biological soil indicator that is rarely applied in the identification of soil quality in coffee farms. The objective was to evaluate edaphic macrofauna and soil physico-chemical properties in four coffee farms at different altitudes. The farms were selected in four hamlets of small-scale coffee farmers. In one-hectare plantations, three monoliths of 25 × 25 cm wide by 30 cm depth were sampled. Soil samples were taken from each plot, then the organic matter (OM) content, hydrogen potential (pH), electrical conductivity (EC) and nitrogen (N) content were determined. There were no differences in macrofaunal diversity for the altitudes studied, but there were differences according to the time of year (rainfall and low water). The maximum Shannon index was 2.2 (rainy season) and 1.1 (dry season). Physico-chemical parameters such as soil pH ranged from 7.8 - 8.15 in the lower altitude farms and for the higher altitude farms it was 6.38 - 6.65. Soil pH was highly negatively correlated with altitude. Nitrogen was positively correlated with organic matter. Faunal diversity is negatively correlated with season and the presence of microorganisms is influenced by the physico-chemical characteristics of the soil.

scholarly journals The Relationship between Differences of Slope Class with Soil Chemical Characteristics in Jolotigo Tea Plantation Scope of PTPN IX

2022 ◽  
Vol 9 (1) ◽  
pp. 171-179
Author(s):  
Pipit Tandyana Febriantika ◽  
Faris Nur Fauzi Athallah ◽  
Restu Wulansari ◽  
Didik Suprayogo
Keyword(s):  
Soil Ph ◽  
Chemical Properties ◽  
Correlation Method ◽  
Soil Nutrient ◽  
Soil Chemical Properties ◽  
Available P ◽  
Subtropical Climate ◽  
Degraded Land ◽  
Total N ◽  
Tea Plantations

Tea plantations are mostly more suitable to be cultivated in areas with highland characteristics to get its’ subtropical climate which is great for the growth of tea. This requirement showed that tea plantations are also cultivated in areas with different ranges of slope and this condition could affect soil chemical properties such as soil nutrient content, including soil pH, soil organic carbon (SOC) and contents of N, Available P, K and Mg inside the soil. This study was conducted to analyze the correlation on different slope levels with soil nutrient contents by collecting the secondary data of land slope and soil chemical properties, analyzed statistically with a simple correlation method. The result showed there was no significant correlation between the slope levels and contents of soil chemical properties. Most of the soil chemical properties have a negative correlation to different slope gradients such as soil pH (r = -0.391), SOC (r = -0.348), total N ( r = -0.169), Available P (r = - 0.039), K content (r = -0.135), Mg content (r = -0.027). where the highest levels of nutrients were found at the lowest level of slope based on the site data. Soil chemical properties are needed to be considered in many tea plantations with different levels of slope and could be used as a recommendation in planning for conservation or restoration of degraded land or soil.

Assessing the Soil Fertility Using Landsat TM Imagery and Geospatial Statistical Analysis

2011 ◽  
Vol 347-353 ◽  
pp. 3559-3563
Author(s):  
Jin Ling Zhao ◽  
Da Cheng Wang ◽  
Dong Yan Zhang ◽  
Ju Hua Luo ◽  
Wen Jiang Huang
Keyword(s):  
Organic Matter ◽  
Soil Fertility ◽  
Soil Ph ◽  
Census Data ◽  
Prediction Models ◽  
Landsat Tm ◽  
Available P ◽  
Support Vector ◽  
Fertility Level ◽  
Total N

This paper aims to investigate the soil fertility of Shunyi District’s cropland combing remote sensing and ground census data based on the Geostatistical Analyst of ArcGIS. Firstly, Landsat TM image was used to identify the spatial distribution and estimate the cropland plot area using support vector machine (SVM) classification method, and the overall classification is 91.5 % by 435 field survey points. Then, the survey indicators were added to ArcGIS such as organic matter, available P, available K, total N, soil pH, etc. After exploring the sample data for each indicator, trend surfaces were generated using the optimum prediction models after cross validation. Finally, according to the identified cropland plots, the soil quality index (SQI) was derived to map the soil fertility of the study area. The result shows that the southwestern part and northeastern corner of this district were found to be high in soil pH, which lies in between 8.2 and 8.6. Additionally, wide variability of organic matter, total N, available P and K were noted which can be due to the extent of cultivation in these areas while the change in fertility level could be due to anthropogenic influence. When considering the soil heavy metals, Zn, Fe, Cu and Mn show almost the same distribution.

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