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Soil Acidity, Organic C, Tota L N, Available Phosphorus and Exchangeable Bases in Some Soils of Tidal Floodplain Region of Bangladesh

M. F. Hoque
Professor, Dept. of SoiI Science, PSTU

M. K. lslam
Assistant Professor, Dept. of SoiI Science, PSTU

M. K. Hossain
Assistant Professor,Dept. of SoiI Science, PSTU

M. S. Hossin
Lecturer, Dept. of SoiI Science, PSTU

M. M. I. Chowdhury
SSO, SRDI Regional Laboratory,Farmgate, Dhaka

Abstract/ Executive Summary:

The distri bution of soil acidity, organic C, available P and exchangeable bases (K Ca, Mg and Na) in the different soil series are related to the growth and development of crop. Some selected tidal floodplain soils of Bangladesh were studied to understand the distribution of soil acidity, organic C, total nitrogen, available P and exchangeable bases . The results revealed that most of the soils are negatively charged . Maximum soils are slightly acidic in reaction and some soils showed slightly alkaline and one soil showed neutral in reaction. Organic C concentration is more or less in most of the soils but two soils showed high organic C. Phosphorus deficiency was observed in most of the soils. Potassium and sodium concentration is below the reported threshold values in most of the soils. Calcium and magnesium concentration of the studied soils is higher in respect of K and Na.

Keywords: Acidity, Available P, Exchangeable bases, Organic C, Total N , Tidal floold plain

Location: Soil Science Laboratory and Central Laboratory of Patuakhali Science and Technology University

Start Date: 00-10-2011

End Date: 00-03-2012

Program Area: Crop-Soil-Water Management

Commodity: Soil fertility

Objectives:

1. To investigate the distribution of soil acidity, organic carbon, total nitrogen , available phosphorus and exchangeable bases in tidal floodplain soils of Bangladesh.

Methodology:

A laboratory experiment was conducted at the Soil Science Laboratory and Central Laboratory of Patuakhali Science and Technology University during the period October 2011 to March 2012 . Thirteen surface (0-15 cm) soil samples used for the sorption study were collected from cultivated rice fields in January to March 2010 after T-Aman harvest. The selected soil sampling sites were of different Upazilla (Dumki, Kalapara , Amtali, Wuzirpur, Gouranadi, Borhanuddin , Lalmohan) of Patuakhali , Borguna, Barisal and Bhola districts . For the convenience of discussion, the 13 soils are referred to as soil 1 through soil 13. The collected soil samples were air-dried and ground to pass a 2-mm sieve. Then the investigations were made with the collected soil sample. Ten grams of air dried soil sample was taken in a 50 ml beaker and 25 ml of distilled water was added. The suspension was stirred with a glass rod at regular interval for 30 minutes. A glass electrode pH meter (SevenEasyTM, pH meter S20, Mettler, Toledo) calibrated with buffer pH 7.0 and 4.0 measured the pH of the soil suspension. The pHKCI was determined by stirring 10 g soil in 25 ml 1.0 M KCI solution in a similar manner of pHw determination. Organic C was determined by Walkely and Black wet digestion method. Total nitrogen was determined by modified Kjeldahl method . Available P was determined by the extracting solution of 0.5 M NaHC0₃, pH 8.5. Exchangeable bases were determined by the extracting solution of I N CH₃COONH₄, pH 7.0.

Source of Information: J. Patukahli Sci and Tech. Univ. 2013, 4(2) : 161 - 171; ISSN 1996-4501

Article Link (Online Journal):

Funding Source:

Total Budget (Tk.) :

Achievement/Findings:

The analysis of tidal floodplain soil of different soil series collected from different locations of coastal region of Bangladesh indicates that the maximum soils are negatively charged. Maximum soils are slightly acidic in reaction and some soils showed slight alkaline and one soil showed neutral in reaction. Organic C concentration is more or less considerable in most of the soils but two soils showed high organic C. Phosphorus deficiency was observed in most of the soils. Potassium concentration is below the reported threshold values and sodium concentration is considerable in most of the soils. Calcium and magnesium concentration of the studied soils is higher in respect of K and Na.

Knowledge Management: Journal