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Research Detail

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M. lahiruddin
Department of Soil Science, Bangladesh Agricultural University, Mymensingh 2202,Bangladesh.

H. Harada
National Grassland Research Institute, Nishinasuno, Tochigi, 329-2793 Japan

T. Hatanaka
National Grassland Research Institute, Nishinasuno, Tochigi, 329-2793 Japan

M.R. Islam
Department of Soil Science, Bangladesh Agricultural University, Mymensingh 2202,Bangladesh.

An investigation was undertaken to examine the levels of various trace elements in agricultural soils of Bangladesh and to analyze their relationship with some soil properties. Trace elements under study included Cu, Zn, Mn, As, Mo, Cd, Sb, and Pb. Forty samples of top soils were collected from farmers' fields in two major agroecological regions (AEZs) of the country_ The two AEZs represented separately non-calcareous (pH around 6.5, free CaC03 absent) and calcareous (pH around 7.6, free CaC03 present) soils. Soil samples were digested with HF-HN03 followed by the determination of the levels of the elements by ICP-MS. Levels of trace elements varied considerably between the locations and soil types. The clay content of the non-calcareous and the organic matter plus clay content of the calcareous soils were mainly responsible for such a variation. The total contents of all the trace elements except for As in calcareous soils were much lower than the maximum acceptable limit for agricultural soils. Generally, the concentration of each trace element in calcareous soils was considerably higher than that in non-calcareous soils. The total amount of trace elements in both non-calcareous and calcareous soils followed the order: Mn>>Zn>Pb, Cu>As>>Mo, Sb>Cd.

  Agricultural soils, Clay, rCP-MS, Organic matter, Trace elements
  Farmers' fields in two agroecological regions (AEZs) of Bangladesh,namely the Old Brahmaputra Floodplain (AEZ9) and High Ganges River Floodplain (AEZ 11)
  00-01-1999
  00-06-1999
  Crop-Soil-Water Management
  Soil fertility

1. To analyze the status of several trace elements viz. Cu, Zn, Mn, As, Mo, Cd, Sb, and Pb in agricultural soils of two major agroecological regions (Old Brahmaputra Floodplain and High Ganges River Floodplain) of Bangladesh which display contrasting soil characteristics.

Forty soil samples at 0-15 cm depth were collected from farmers' fields in two agroecological regions (AEZs) of Bangladesh, namely the Old Brahmaputra Floodplain (AEZ9) and High Ganges River Floodplain (AEZ 11). The two AEZs display contrasting soil characteristics, the AEZ9 soils being non-calcareous (pH around 6.5, free CaC03 absent) and the AEZII soils being calcareous (pH around 7.6, free CaC03 present). The crops grown in the AEZ9 are mainly rice followed by wheat, mustard, and pulses, while in the AEZII, apart from rice-based cropping patterns, sugarcane is cultivated alone. In this cultivation, normal agricultural practices such as irrigation, fertilizer application, manuring, pesticide spray, etc. are adopted. The soils were collected based on the soil texture and land type. The soils were air-dried, ground, and passed through a 2-mm sieve. For trace element analysis, the soils were further ground to a fine powder « 0.1 mm) using a tungsten-carbide vibration mill. Soil samples in duplicate were analyzed for trace elements along with the pH, organic matter, and clay contents. The soil pH (H20) was determined by using a pH meter with a glass electrode, the clay content using a hydrometer and the organic matter content by the wet oxidation method. Soil samples weighing 0.1 g were taken into a Teflon tube. Into the tube, 1 mL HN03, 0.5 mL HF, and 0.1 mL HCI04 were added. The Teflon tubes were placed on an aluminium block heater, and then the temperature of the block was raised slowly to about 120T. Heating was continued until HF was completely evaporated. Then 0.1 mL of HCI04 was added and the tubes were heated until the acid material was evaporated leaving the residue dry. The dry residue in the tube was dissolved with 15 mL of base solution containing indium (50 ppb) and conc. HN03 (15 mL L -1). It took altogether 16 h to obtain a complete digestion. The contents of the elements were determined by inductively coupled plasma mass spectroscopy (ICP-MS, Model SPQ8000, Seiko Instruments Co., Chiba, Japan). Multi-element standard solutions, XTC-22 and XTC-I07 (SPEX Industries Inc., Edison, USA) were used for preparing different standards of the elements, Cu, Zn, Mn, As, Mo, Cd, Sb, and Pb with atomic mass number 63, 66, 55, 75, 98, 114, 121, and 208, respectively. Indium was used as an internal standard for the correction of ICP-MS instrumental drift and matrix effects.

  Soil Sci. Plant Nutr., 46 (4), 963-968, 2000
  
Funding Source:
  

The total contents of all the trace elements except for As in calcareous soils were much lower than the maximum acceptable limit for agricultural soils. Generally, the concentration of each trace element in calcareous soils was considerably higher than that in non-calcareous soils. The total amount of trace elements in both non-calcareous and calcareous soils followed the order: Mn>>Zn>Pb, Cu>As>>Mo, Sb>Cd.

  Journal
  


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