K-Dynamics in a Continuously Submerged Limed and the Corresponding Unlimed Soil Subjected to One and Two Cycles of Drying Phase

Tapa Debnath; Sayan Majumder; Dipankar Saha

doi:doi:10.11648/j.ajac.20180606.11

| Peer-Reviewed

K-Dynamics in a Continuously Submerged Limed and the Corresponding Unlimed Soil Subjected to One and Two Cycles of Drying Phase

Tapa Debnath, Sayan Majumder, Dipankar Saha

Published in American Journal of Applied Chemistry (Volume 6, Issue 6)

Received: 9 December 2018 Accepted: 3 January 2019 Published: 31 January 2019

Views: Downloads:

Download PDF

Share This Article

Twitter
Linked In
Facebook

Abstract

A laboratory experiment was carried out to study the effect of drying phases on transformation of different fractions of K in submerged limed and the corresponding unlimed soil in presence and absence of N and K fertilizers. Changes in different fractions of K were monitored with time. Results showed that irrespective of treatments, available K increased in the limed soil throughout the period of incubation. However, non-exchangeable K showed an exactly opposite trend of results particularly in limed situation indicating a dynamic equilibrium between these forms of K in soils. Although, the trend of results of both available and non-exchangeable forms are totally different in unlimed situation. The decrease in 1N boiling HNO3 extractable K is comparatively more in limed soil subjected to single drying phase. No drastic variation in lattice and total K is observed under different treatment combinations. It indicates, maintenance of drying phase has little effect on lattice and total K in soils.

Published in	American Journal of Applied Chemistry (Volume 6, Issue 6)
DOI	10.11648/j.ajac.20180606.11
Page(s)	189-196
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Different Forms of K, Drying Phases, Liming, Submerged Soil, N and K Fertilizers

References

[1]	BhaleraoVP, Deshpandeb AN, Bansal SK. (2018). Potassium Dynamics in Inceptisols as Influenced by Graded Levels of Potash for Banana: I. Potassium Fractions. Communications in Soil Science and Plant analysis. 49(2):1-10.
[2]	Weil RR, Brady NC. (2017). The Nature and Properties of Soils (15th Edition) Pearson Education Limited, Harlow, England.
[3]	Qiu S, Xie J, Zhao S, Xu X, Hou Y, Wang X, Zhou W, He P, Johnston AM, Christie P, Jin J. (2014) Long-term effects of potassium fertilization on yield, efficiency, and soil fertility status in a rain-fed maize system in northeast China. Field Crops Research 163: 1–9.
[4]	Bhattacharyya K, Das T, Ray K, Dutta S, Majumdar, K, Pari A, Banerjee H. (2018). Yield of and nutrient-water use by maize exposed to moisture stress and K fertilizers in an inceptisol of West Bengal, India. Agricultural Water Management 206: 31–41.
[5]	Steiner F, Lana MDC, Zoz1 T, Frandoloso JF. (2015). Changes in potassium pools in Paraná soils under successive cropping and potassium fertilization. Semina: Ciências Agrárias, Londrina, 36(6):2. p 4083-4098.
[6]	Lalitha M, Dhakshinamoorthy M. (2014). Forms of Soil Potassium-A Review. Agriultural Reviews. 35(1): 64-68.
[7]	Havlin, JL, Tisdale SL, Beaton JD, Nelson WL, (2016) Soil Fertility and Fertilizers: An Introduction to Nutrient Management (8th Edition) Pearson Educational, Inc. New Delhi.
[8]	Habib F, Javid S, Saleem I, Ehsan S, and Ahmad Z A. (2014). Potassium dynamics in soil under long term regimes of organic and inorganic fertilizer application. Soil Environ. 33(2): 110-115.
[9]	Majumdar K, Sanyal SK, Singh VK, Dutta S, Satyanarayana T, Dwivedi BS. (2017). Potassium Fertiliser Management in Indian.
[10]	Tripura S, Majumder S, Saha D. (2017). Transformation of different fractions of K in a limed and the unlimed soil treated with and without organic matter as well as N and K fertilizers. The Bioscan. 12(2): 1029-1034.
[11]	Das R, Saha D. (2013). Changes in non-exchangeable K in an acid and the corresponding limed soil as affected by addition of nitrogenous and potassic fertilizers. Journal of Crop and Weed, 9(1):99-102.
[12]	Tripura S, Majumder S, Saha D. (2016). Transformations of different fractions of K in a limed and the corresponding unlimed soil in presence and absence of N and K fertilizers. Agrochimica. 60(4): 262-274.
[13]	Oustan S, Asghari M, Neyshabouri MR, Bybordi A. (2008). Potassium Fixation as Affected by Moisture Conditions in Some Soils of Azerbaijan. In: Proceedings of International Meeting on Soil Fertility Land Management and Agroclimatology. Turkey, p:619-625.
[14]	Jha, SK, Jha AK, Ojha RK, Kumar R. (2011). Potassium fixation as affected by alternate wetting and drying in some soil series of Jharkhand. Asian journal of Soil Science. 6(2): 181-184.
[15]	Shoemaker HE, Mclean EO, Pratt PF. (1961). Buffer methods for derermining lime requirement of soils with appreciable amounts of extractable aluminum. Soil Science Society of America Proceedings. 25: 274-277.
[16]	Bouyoucos GJ. (1962). Hydrometer method improved for making particle size analysis of soils. Agronomy Journal. 54: 464-465.
[17]	Piper, C. S. (1942). Soil and Plant Analysis: a laboratory manual of methods for the examinations of soils and the determination of the inorganic constituents of plants. University of Adelaide, Adelaide.
[18]	Black, C. A. (1965). Method of Soil Analysis. Part 2. Chemical and Microbiological Properties. American Society of Agronomy, Inc. Publisher, Madison, Wisconsin, USA.
[19]	Jackson ML. (1973). Soil Chemical Analysis. Prentice Hall of India Pvt. Ltd. New Delhi.
[20]	Walkley A, Black IA. (1934). An examination of wet acid method for determining soil organic matter and a proposed modification of the chromic acid titration method. Soil Science. 37: 29-38.
[21]	Bremner JM, Keeney DR. (1966). Determination of exchangeable ammonia, nitrate and nitrite by extraction distillation methods. Soil Science Society of America Proceedings. 30: 577-587.
[22]	Bremner J. (1965). In: Methods of Soil Analysis. Part 2. (C.A. Black Ed.) American Society of Agronomy, Madison, Wisconsin, USA. pp. 1149-1162.
[23]	Bray RH, Kurtz, LT. (1945). Determination of total, organic and available forms of phosphorus in soils. Soil Science. 59: 39-45.
[24]	Olsen SR, Cole CV, Watnabe FS, Dean LA. (1954). Estimation of available phosphorus in soils by extraction with sodiumbicarbonate. US Dept. Agriculture Circular. 93.
[25]	Sarkar GK, Chattopadhyay AP, Sanyal, SK. (2013). Release pattern of non-exchangeable potassium reserves in Alfisols, Inceptisols and Entisols of West Bengal, India. Geoderma. 207–208(1):8–14.
[26]	Das R, Saha D. (2014). Effect of liming on the changes of different forms of potassium in an acid soil treated with N and K fertilizers. Journal of the Indian Chemical Society. 91: 1619-1625.
[27]	Sarkar GK, Debnath A, Chattopadhyay AP, Sanyal, SK. (2014). Depletion of Soil Potassium under Exhaustive Cropping in Inceptisol and Alfisol. Communications in Soil Science and Plant Analysis, 45:61–72.
[28]	Habib F, Javid S, Saleem I, Ehsan S, Ahmed ZA. (2014). Potassium dynamics in soil under long term regimes of organic and inorganic fertilizer application. Soil & Environment. 33: 110-115.

Cite This Article

Plain Text BibTeX RIS

APA Style

Tapa Debnath, Sayan Majumder, Dipankar Saha. (2019). K-Dynamics in a Continuously Submerged Limed and the Corresponding Unlimed Soil Subjected to One and Two Cycles of Drying Phase. American Journal of Applied Chemistry, 6(6), 189-196. https://doi.org/10.11648/j.ajac.20180606.11

Copy | Download

ACS Style

Tapa Debnath; Sayan Majumder; Dipankar Saha. K-Dynamics in a Continuously Submerged Limed and the Corresponding Unlimed Soil Subjected to One and Two Cycles of Drying Phase. Am. J. Appl. Chem. 2019, 6(6), 189-196. doi: 10.11648/j.ajac.20180606.11

Copy | Download

AMA Style

Tapa Debnath, Sayan Majumder, Dipankar Saha. K-Dynamics in a Continuously Submerged Limed and the Corresponding Unlimed Soil Subjected to One and Two Cycles of Drying Phase. Am J Appl Chem. 2019;6(6):189-196. doi: 10.11648/j.ajac.20180606.11

Copy | Download

@article{10.11648/j.ajac.20180606.11,
  author = {Tapa Debnath and Sayan Majumder and Dipankar Saha},
  title = {K-Dynamics in a Continuously Submerged Limed and the Corresponding Unlimed Soil Subjected to One and Two Cycles of Drying Phase},
  journal = {American Journal of Applied Chemistry},
  volume = {6},
  number = {6},
  pages = {189-196},
  doi = {10.11648/j.ajac.20180606.11},
  url = {https://doi.org/10.11648/j.ajac.20180606.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajac.20180606.11},
  abstract = {A laboratory experiment was carried out to study the effect of drying phases on transformation of different fractions of K in submerged limed and the corresponding unlimed soil in presence and absence of N and K fertilizers. Changes in different fractions of K were monitored with time. Results showed that irrespective of treatments, available K increased in the limed soil throughout the period of incubation. However, non-exchangeable K showed an exactly opposite trend of results particularly in limed situation indicating a dynamic equilibrium between these forms of K in soils. Although, the trend of results of both available and non-exchangeable forms are totally different in unlimed situation. The decrease in 1N boiling HNO3 extractable K is comparatively more in limed soil subjected to single drying phase. No drastic variation in lattice and total K is observed under different treatment combinations. It indicates, maintenance of drying phase has little effect on lattice and total K in soils.},
 year = {2019}
}

Copy | Download

TY  - JOUR
T1  - K-Dynamics in a Continuously Submerged Limed and the Corresponding Unlimed Soil Subjected to One and Two Cycles of Drying Phase
AU  - Tapa Debnath
AU  - Sayan Majumder
AU  - Dipankar Saha
Y1  - 2019/01/31
PY  - 2019
N1  - https://doi.org/10.11648/j.ajac.20180606.11
DO  - 10.11648/j.ajac.20180606.11
T2  - American Journal of Applied Chemistry
JF  - American Journal of Applied Chemistry
JO  - American Journal of Applied Chemistry
SP  - 189
EP  - 196
PB  - Science Publishing Group
SN  - 2330-8745
UR  - https://doi.org/10.11648/j.ajac.20180606.11
AB  - A laboratory experiment was carried out to study the effect of drying phases on transformation of different fractions of K in submerged limed and the corresponding unlimed soil in presence and absence of N and K fertilizers. Changes in different fractions of K were monitored with time. Results showed that irrespective of treatments, available K increased in the limed soil throughout the period of incubation. However, non-exchangeable K showed an exactly opposite trend of results particularly in limed situation indicating a dynamic equilibrium between these forms of K in soils. Although, the trend of results of both available and non-exchangeable forms are totally different in unlimed situation. The decrease in 1N boiling HNO3 extractable K is comparatively more in limed soil subjected to single drying phase. No drastic variation in lattice and total K is observed under different treatment combinations. It indicates, maintenance of drying phase has little effect on lattice and total K in soils.
VL  - 6
IS  - 6
ER  -

Copy | Download

Author Information

Tapa Debnath

Department of Agricultural Chemistry and Soil Science, Faculty of Agriculture, Bidhan Chandra Krishi Viswavidyalaya, Mohanpur, India
Sayan Majumder

Department of Agricultural Chemistry and Soil Science, Faculty of Agriculture, Bidhan Chandra Krishi Viswavidyalaya, Mohanpur, India
Dipankar Saha

Department of Agricultural Chemistry and Soil Science, Faculty of Agriculture, Bidhan Chandra Krishi Viswavidyalaya, Mohanpur, India

Download PDF

Sections

Plain Text BibTeX RIS

APA Style

Tapa Debnath, Sayan Majumder, Dipankar Saha. (2019). K-Dynamics in a Continuously Submerged Limed and the Corresponding Unlimed Soil Subjected to One and Two Cycles of Drying Phase. American Journal of Applied Chemistry, 6(6), 189-196. https://doi.org/10.11648/j.ajac.20180606.11

Copy | Download

ACS Style

Tapa Debnath; Sayan Majumder; Dipankar Saha. K-Dynamics in a Continuously Submerged Limed and the Corresponding Unlimed Soil Subjected to One and Two Cycles of Drying Phase. Am. J. Appl. Chem. 2019, 6(6), 189-196. doi: 10.11648/j.ajac.20180606.11

Copy | Download

AMA Style

Tapa Debnath, Sayan Majumder, Dipankar Saha. K-Dynamics in a Continuously Submerged Limed and the Corresponding Unlimed Soil Subjected to One and Two Cycles of Drying Phase. Am J Appl Chem. 2019;6(6):189-196. doi: 10.11648/j.ajac.20180606.11

Copy | Download

@article{10.11648/j.ajac.20180606.11,
  author = {Tapa Debnath and Sayan Majumder and Dipankar Saha},
  title = {K-Dynamics in a Continuously Submerged Limed and the Corresponding Unlimed Soil Subjected to One and Two Cycles of Drying Phase},
  journal = {American Journal of Applied Chemistry},
  volume = {6},
  number = {6},
  pages = {189-196},
  doi = {10.11648/j.ajac.20180606.11},
  url = {https://doi.org/10.11648/j.ajac.20180606.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajac.20180606.11},
  abstract = {A laboratory experiment was carried out to study the effect of drying phases on transformation of different fractions of K in submerged limed and the corresponding unlimed soil in presence and absence of N and K fertilizers. Changes in different fractions of K were monitored with time. Results showed that irrespective of treatments, available K increased in the limed soil throughout the period of incubation. However, non-exchangeable K showed an exactly opposite trend of results particularly in limed situation indicating a dynamic equilibrium between these forms of K in soils. Although, the trend of results of both available and non-exchangeable forms are totally different in unlimed situation. The decrease in 1N boiling HNO3 extractable K is comparatively more in limed soil subjected to single drying phase. No drastic variation in lattice and total K is observed under different treatment combinations. It indicates, maintenance of drying phase has little effect on lattice and total K in soils.},
 year = {2019}
}

Copy | Download

TY  - JOUR
T1  - K-Dynamics in a Continuously Submerged Limed and the Corresponding Unlimed Soil Subjected to One and Two Cycles of Drying Phase
AU  - Tapa Debnath
AU  - Sayan Majumder
AU  - Dipankar Saha
Y1  - 2019/01/31
PY  - 2019
N1  - https://doi.org/10.11648/j.ajac.20180606.11
DO  - 10.11648/j.ajac.20180606.11
T2  - American Journal of Applied Chemistry
JF  - American Journal of Applied Chemistry
JO  - American Journal of Applied Chemistry
SP  - 189
EP  - 196
PB  - Science Publishing Group
SN  - 2330-8745
UR  - https://doi.org/10.11648/j.ajac.20180606.11
AB  - A laboratory experiment was carried out to study the effect of drying phases on transformation of different fractions of K in submerged limed and the corresponding unlimed soil in presence and absence of N and K fertilizers. Changes in different fractions of K were monitored with time. Results showed that irrespective of treatments, available K increased in the limed soil throughout the period of incubation. However, non-exchangeable K showed an exactly opposite trend of results particularly in limed situation indicating a dynamic equilibrium between these forms of K in soils. Although, the trend of results of both available and non-exchangeable forms are totally different in unlimed situation. The decrease in 1N boiling HNO3 extractable K is comparatively more in limed soil subjected to single drying phase. No drastic variation in lattice and total K is observed under different treatment combinations. It indicates, maintenance of drying phase has little effect on lattice and total K in soils.
VL  - 6
IS  - 6
ER  -

Copy | Download