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Distribution of total nitrogen in soils of the tropical highlands of Cameroon

(2023) EURASIAN SOIL SCIENCE. 56(7). p.889-901
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Abstract
Understanding the factors controlling soil total N (TN) is helpful in simulating N cycling at local and regional scales. This study was conducted with the aim to; (i) understand the distribution of TN in specific soil horizons (A and B horizons) of three reference soil groups: Acrisols, Cambisols and Ferralsols, common in humid tropical environments, and (ii) to identify factors controlling TN variations among the various soil groups. Twenty-eight Acrisols, 21 Cambisols and 8 Ferralsols profiles spanning a wide range of precipitation gradients, vegetation type/land use and parent materials, from the Northwestern Highlands (NWH) of Cameroon were considered. Soil properties were analyzed following standard procedures. TN had very high coefficients of variation (>35%) in all the reference soil groups (RSGs), with highest mean TN (0.31 +/- 0.03%) observed in the A horizons of Acrisols and the lowest (0.05 +/- 0.01%) in B horizons of Ferralsols. Variations in TN content were significantly (p < 0.05) influenced by parent material, land use type, precipitation and slope gradient. In surface (A) horizons of all the RSGs, TN correlated positively and significantly with clay (p < 0.05), silt (p < 0.01) and soil organic carbon (SOC) (p < 0.01), and negatively with sand (p < 0.01). This observation was slightly different in subsurface (B) horizons. This study provides data which contributes to a better understanding of soil fertility in tropical highlands.
Keywords
Soil Chemistry, Soil Fertility, Tropical Soils, Western Africa, soil fertility, Acrisols, Cambisols, Ferralsols, tropical soils, ORGANIC-CARBON, FOREST ECOSYSTEM, CROP-ROTATION, LAND-USE, AVAILABILITY, MINERALIZATION, FERTILIZATION, PRECIPITATION, RETENTION, AMMONIUM

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Citation

Please use this url to cite or link to this publication:

MLA
Kome, G. K., et al. “Distribution of Total Nitrogen in Soils of the Tropical Highlands of Cameroon.” EURASIAN SOIL SCIENCE, vol. 56, no. 7, 2023, pp. 889–901, doi:10.1134/s1064229322602682.
APA
Kome, G. K., Kips, Ph. A., Yerima, B. P. K., Enang, R. K., & Van Ranst, E. (2023). Distribution of total nitrogen in soils of the tropical highlands of Cameroon. EURASIAN SOIL SCIENCE, 56(7), 889–901. https://doi.org/10.1134/s1064229322602682
Chicago author-date
Kome, G. K., Ph. A. Kips, B. P. K. Yerima, R. K. Enang, and Eric Van Ranst. 2023. “Distribution of Total Nitrogen in Soils of the Tropical Highlands of Cameroon.” EURASIAN SOIL SCIENCE 56 (7): 889–901. https://doi.org/10.1134/s1064229322602682.
Chicago author-date (all authors)
Kome, G. K., Ph. A. Kips, B. P. K. Yerima, R. K. Enang, and Eric Van Ranst. 2023. “Distribution of Total Nitrogen in Soils of the Tropical Highlands of Cameroon.” EURASIAN SOIL SCIENCE 56 (7): 889–901. doi:10.1134/s1064229322602682.
Vancouver
1.
Kome GK, Kips PhA, Yerima BPK, Enang RK, Van Ranst E. Distribution of total nitrogen in soils of the tropical highlands of Cameroon. EURASIAN SOIL SCIENCE. 2023;56(7):889–901.
IEEE
[1]
G. K. Kome, Ph. A. Kips, B. P. K. Yerima, R. K. Enang, and E. Van Ranst, “Distribution of total nitrogen in soils of the tropical highlands of Cameroon,” EURASIAN SOIL SCIENCE, vol. 56, no. 7, pp. 889–901, 2023.
@article{01H0FPZ94KP7J8JBTYZC8ZZ039,
  abstract     = {{Understanding the factors controlling soil total N (TN) is helpful in simulating N cycling at local and regional scales. This study was conducted with the aim to; (i) understand the distribution of TN in specific soil horizons (A and B horizons) of three reference soil groups: Acrisols, Cambisols and Ferralsols, common in humid tropical environments, and (ii) to identify factors controlling TN variations among the various soil groups. Twenty-eight Acrisols, 21 Cambisols and 8 Ferralsols profiles spanning a wide range of precipitation gradients, vegetation type/land use and parent materials, from the Northwestern Highlands (NWH) of Cameroon were considered. Soil properties were analyzed following standard procedures. TN had very high coefficients of variation (>35%) in all the reference soil groups (RSGs), with highest mean TN (0.31 +/- 0.03%) observed in the A horizons of Acrisols and the lowest (0.05 +/- 0.01%) in B horizons of Ferralsols. Variations in TN content were significantly (p < 0.05) influenced by parent material, land use type, precipitation and slope gradient. In surface (A) horizons of all the RSGs, TN correlated positively and significantly with clay (p < 0.05), silt (p < 0.01) and soil organic carbon (SOC) (p < 0.01), and negatively with sand (p < 0.01). This observation was slightly different in subsurface (B) horizons. This study provides data which contributes to a better understanding of soil fertility in tropical highlands.}},
  author       = {{Kome, G. K. and Kips, Ph. A. and Yerima, B. P. K. and Enang, R. K. and Van Ranst, Eric}},
  issn         = {{1064-2293}},
  journal      = {{EURASIAN SOIL SCIENCE}},
  keywords     = {{Soil Chemistry,Soil Fertility,Tropical Soils,Western Africa,soil fertility,Acrisols,Cambisols,Ferralsols,tropical soils,ORGANIC-CARBON,FOREST ECOSYSTEM,CROP-ROTATION,LAND-USE,AVAILABILITY,MINERALIZATION,FERTILIZATION,PRECIPITATION,RETENTION,AMMONIUM}},
  language     = {{eng}},
  number       = {{7}},
  pages        = {{889--901}},
  title        = {{Distribution of total nitrogen in soils of the tropical highlands of Cameroon}},
  url          = {{http://doi.org/10.1134/s1064229322602682}},
  volume       = {{56}},
  year         = {{2023}},
}

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