Iron and Calcium Availability to Groundnut Plants as Affected by Calcium Carbonate and Water Levels in Calcareous Soil

2008 ◽  
Vol 21 (2) ◽  
pp. 209-220
Author(s):  
Reshmi Sarkar ◽  
B. Basavaraj ◽  
Sandipta Kar
2016 ◽  
Vol 216 ◽  
pp. 1-11 ◽  
Author(s):  
Zhimiao Zhao ◽  
Xinshan Song ◽  
Wei Wang ◽  
Yanping Xiao ◽  
Zhijie Gong ◽  
...  

1990 ◽  
Vol 8 (1) ◽  
pp. 1-4
Author(s):  
G. Kidder ◽  
M.J. Holsinger ◽  
T.H. Yeager

Abstract Wettable sulfur (S) mixed with a Pineda fine sand (an Arenic Glossaqualf with 7.8 pH and 1.5% calcium carbonate equivalent) quickly acidified the soil, but the effect was lost within 8 weeks at low application rates and within 21 weeks at the highest rate (1 g S/kg soil or 1 lb S/1000 lb soil). Granular S mixed with the soil took one year to produce maximum pH reduction of 0.3, 0.4, and 0.9 pH units at 250, 500, and 1000 mg S/kg soil (1/4, 1/2, and 1 lb S/1000 lb soil), respectively . Wettable sulfur (S), surface-applied at 100 g/m2 (0.036 oz/10 ft2), lowered the pH of the upper 5 cm (2 in) of soil to the 5.6 to 5.8 range for one to two months before the pH returned to > 7.0; granular S took about five months to lower the pH to 6.7 but the soil pH was 6.2 two years after application. Wettable S at 20 g/kg soil (0.32 oz S/lb soil) in a small cylindrical zone resulted in a temporary depression of pH within the treated zone but had no effect on pH in other areas of the container. Mixing up to 1.0 g iron sulfate/kg soil (0.016 oz/lb soil) failed to reduce soil pH. Live-oak trunk diameter and plant height were not affected by any of the soil treatments in the two-year experiment.


2017 ◽  
Vol 225 ◽  
pp. 262-271 ◽  
Author(s):  
Zhao Zhimiao ◽  
Song Xinshan ◽  
Zhao Yufeng ◽  
Xiao Yanping ◽  
Wang Yuhui ◽  
...  

2009 ◽  
Vol 228 (5) ◽  
pp. 789-797 ◽  
Author(s):  
Carmen Frontela ◽  
Gaspar Ros ◽  
Carmen Martínez

2021 ◽  
Vol 2 (1) ◽  
pp. 1-4
Author(s):  
Ideisan I Abu-Abdoun

Calcareous soil that contains enough free calcium carbonate to effervesce visibly, releasing carbon-dioxide gas, when treated with diluted sulfuric acid. Analysis of calcareous soil in Jordan valley after treatment with aqueous low concentration sulfuric acid shows some change in the physical prosperities of the soil such as reduction of calcium carbonate from 66% to 30%, soil density from 1.60 g/cm3 to 1.19 g/cm3 . Soil texture is convert from silt clay loam to silt loam this physical changing makes soil permeability is easier so it could be suitable for agricultural without effect in plant growth also we show reduce soil PH and increasing in soil filtration tare. We showed several changes in the plants, which planted in the treated soil by sulfuric acid as increasing in the product from 10 - 25 %, would reduce in using chemical fertilizers from 15-30% and absence of soil diseases.


2015 ◽  
Vol 63 (2) ◽  
pp. 102-109 ◽  
Author(s):  
Ahmad Farrokhian Firouzi ◽  
Mehdi Homaee ◽  
Erwin Klumpp ◽  
Roy Kasteel ◽  
Wolfgang Tappe

Abstract Study of bacterial transport and retention in soil is important for various environmental applications such as groundwater contamination and bioremediation of soil and water. The main objective of this research was to quantitatively assess bacterial transport and deposition under saturated conditions in calcareous soil. A series of leaching experiments was conducted on two undisturbed soil columns. Breakthrough curves of Pseudomonas fluorescens and Cl were measured. After the leaching experiment, spatial distribution of bacteria retention in the soil columns was determined. The HYDRUS-1D one- and two-site kinetic models were used to predict the transport and deposition of bacteria in soil. The results indicated that the two-site model fits the observed data better than one-site kinetic model. Bacteria interaction with the soil of kinetic site 1 revealed relatively fast attachment and slow detachment, whereas attachment to and detachment of bacteria from kinetic site 2 was fast. Fast attachment and slow detachment of site 1 can be attributed to soil calcium carbonate that has favorable attachment sites for bacteria. The detachment rate was less than 0.02 of the attachment rate, indicating irreversible attachment of bacteria. High reduction rate of bacteria was also attributed to soil calcium carbonate.


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