International Journal of Environmental Science and Development

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Volume 15 Number 4 (2024)

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IJESD 2024 Vol.15(4): 169-175
doi: 10.18178/ijesd.2024.15.4.1482

Estimation of Carbon Stocks on Difference Land Use and Slopes in The Central of Horticultural Production Banuhampu Agam, West Sumatra Indonesia

Syafrimen Yasin1, Amsar Maulana2, Iwan Darfis1, Fachrul Razi3, Dewi Rezki4, Ellsya Tatalia Augustin Putri Tanjung3, Tasya Rahmatul Zalfi3, Yesma Melly Mailiza4, and Herviyanti Herviyanti1,*
1Department of Soil Science and Land Resources, Agriculture Faculty, Andalas University, Limau Manis, Padang City, 25164, Indonesia
2Doctoral Program of Agricultural Science, Postgraduate of Agriculture Faculty Andalas University, Limau Manis, Padang City, 25164, Indonesia
3Bachelor Program of Soil Science, Agriculture Faculty Andalas University, Limau Manis, Padang City, 25164, Indonesia
4Department of Agroecotechnology, Agriculture Faculty, Andalas University, Pulau Punjung Dharmasraya, 27573, Indonesia
Email: syafrimenyasin@agr.unand.ac.id (S.Y.); amaulana.1005@gmail.com (A.M.); irwandarfis_dd@yahoo.co.id (I.D.); fachrulrazi376@gmail.com (F.R.); dewirezki@agr.unand.ac.id (D.R.); ellsyatatalia0908@gmail.com (E.T.A.P.T.); tasyazalfi8@gmail.com (T.R.Z.); mellymailizayesma@gmail.com (Y.M.M.); herviyanti@agr.unand.ac.id (H.H.)
*Corresponding author
Manuscript received December 11, 2023; revised February 2, 2024; accepted April 1, 2024; published July 15, 2024

Abstract—Soil Organic Carbon (SOC) has an important role in soil fertility, so it becomes one of the soil properties as an indicator in determining soil health and quality. The amount of carbon stock in the soil can change due to land use and erosion that occurs at different slope levels and the transformation process from soil to air in the form of CO2, which can cause global warming. This study aims to study soil carbon stocks in various types of land use and slope levels at The Central of Horticultural Production, Banuhampu Agam West Sumatra. Soil sampling from various types of land use (forest, paddy fields, and fields) and slope (0–8; 8–15; 15–25, and 25–45%) at a depth of 0–20 cm. The results showed that the average value of BD and SOC at The Central of Horticultural Production, Banuhampu Agam West Sumatra, was 0.93 g cm−3 and 0.22% C with a carbon potential of 4.04E2 Mg ha−1. The highest estimation of soil carbon stocks on land use and slopes in The Central of Horticultural Production of 296338.76 [paddy (0– 8%)]; 118778.52 [fields (15–25%)]; and 55367.64 [forest (25– 45%)] Mg. The Correlation of soil carbon stock in The Central of Horticultural Production, Banuhampu Agam West Sumatra, is positively related to carbon potential = carbon density > bulk density > SOC (r = 0.111 = 0.111 > 0.094 > 0.048).

Keywords—carbon stocks, land use, slopes, horticultural production

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Cite: Syafrimen Yasin, Amsar Maulana, Iwan Darfis, Fachrul Razi, Dewi Rezki, Ellsya Tatalia Augustin Putri Tanjung, Tasya Rahmatul Zalfi, Yesma Melly Mailiza, and Herviyanti Herviyanti, "Estimation of Carbon Stocks on Difference Land Use and Slopes in The Central of Horticultural Production Banuhampu Agam, West Sumatra Indonesia, " International Journal of Environmental Science and Development vol. 15, no. 4, pp. 169-175, 2024.

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