Potensi Serapan Karbon Inorganik pada Kawasan Karst Tropis di Karst Biduk-Biduk, Kalimantan Timur

Danardono Danardono; Eko Haryono; M Widyastuti

doi:10.14710/jwl.10.3.267-281

DOI: https://doi.org/10.14710/jwl.10.3.267-281

Potensi Serapan Karbon Inorganik pada Kawasan Karst Tropis di Karst Biduk-Biduk, Kalimantan Timur

*Danardono Danardono

- Fakultas Geografi, Universitas Muhammadiyah Surakarta, Indonesia

Eko Haryono - Fakultas Geografi, Universitas Gadjah Mada, Yogyakarta, Indonesia

M Widyastuti - Fakultas Geografi, Universitas Gadjah Mada, Yogyakarta, Indonesia

This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License.

BibTex Citation Data :

@article{JWL12256,
    author = {Danardono Danardono and Eko Haryono and M Widyastuti},
    title = {Potensi Serapan Karbon Inorganik pada Kawasan Karst Tropis di Karst Biduk-Biduk, Kalimantan Timur},
    journal = {Jurnal Wilayah dan Lingkungan},
  volume = {10},
    number = {3},
    year = {2022},
    keywords = {carbon sequestration; dissolution rate; inorganic carbon; karst; limestone tablets},
    abstract = {The increase in carbon emissions in Indonesia is a problem that needs to be mitigated. One of the ways is to make an inventory of areas that have the potential to absorb carbon. One of areas that has the potential to absorb inorganic carbon is the karst area through the karstification process. However, research on inorganic carbon sequestration in karst areas, especially in tropical karst areas, is rarely studied. This potential needs to be studied to determine the important role of karst areas in efforts to reduce global carbon emissions. This study aims to identify the potential value of inorganic carbon sequestration; in Biduk-Biduk Karst Area and this efforts to reduce carbon emissions in Indonesia. Inorganic carbon sequestration was calculated based on the dissolution rate of carbonate rocks using standard limestone tablets. The efforts of karst areas to reduce carbon emissions was modeled by comparing the total value of inorganic carbon sequestration in karst areas with the value of carbon emissions in Indonesia. The results showed that the potential of the Biduk-Biduk Tropical Karst to absorb inorganic carbon is 726.864 tons/year-CO2. Inorganic carbon uptake shows variation based on differences in surface morphology, where areas with flat slopes have a higher inorganic carbon sequestrationn. This value can help to reduce carbon emissions in East Kalimantan by 7.3% and Indonesia by 0.5%. Therefore, conservation of karst areas is important to do to support carbon emission reduction programs in Indonesia.},
   issn = {2407-8751},   pages = {267--281}  doi = {10.14710/jwl.10.3.267-281},
    url = {https://ejournal2.undip.ac.id/index.php/jwl/article/view/12256}
}

Citation Format:

Abstract

The increase in carbon emissions in Indonesia is a problem that needs to be mitigated. One of the ways is to make an inventory of areas that have the potential to absorb carbon. One of areas that has the potential to absorb inorganic carbon is the karst area through the karstification process. However, research on inorganic carbon sequestration in karst areas, especially in tropical karst areas, is rarely studied. This potential needs to be studied to determine the important role of karst areas in efforts to reduce global carbon emissions. This study aims to identify the potential value of inorganic carbon sequestration; in Biduk-Biduk Karst Area and this efforts to reduce carbon emissions in Indonesia. Inorganic carbon sequestration was calculated based on the dissolution rate of carbonate rocks using standard limestone tablets. The efforts of karst areas to reduce carbon emissions was modeled by comparing the total value of inorganic carbon sequestration in karst areas with the value of carbon emissions in Indonesia. The results showed that the potential of the Biduk-Biduk Tropical Karst to absorb inorganic carbon is 726.864 tons/year-CO2. Inorganic carbon uptake shows variation based on differences in surface morphology, where areas with flat slopes have a higher inorganic carbon sequestrationn. This value can help to reduce carbon emissions in East Kalimantan by 7.3% and Indonesia by 0.5%. Therefore, conservation of karst areas is important to do to support carbon emission reduction programs in Indonesia.

Fulltext View|Download

Keywords: carbon sequestration; dissolution rate; inorganic carbon; karst; limestone tablets

Article Metrics:

Article Info

Section: Research Articles

Language : ID

In Vol 10, No 3 (2022): December 2022

Recent articles

Potensi Serapan Karbon Inorganik pada Kawasan Karst Tropis di Karst Biduk-Biduk, Kalimantan Timur Konsep Pengembangan Desa Wisata Pesisir Tangguh Bencana Berbasis Perencanaan Ruang [Studi Kasus: Desa Kunjir, Kabupaten Lampung Selatan] Validasi Instrumen Indeks Kota Berkelanjutan dengan Analisis Faktor More recent articles

Akiyama, S., Hattanji, T., Matsushi, Y., & Matsukura, Y. (2015). Dissolution rates of subsoil limestone in a doline on the Akiyoshi-dai Plateau, Japan: An approach from a weathering experiment, hydrological observations, and electrical resistivity tomography. Geomorphology, 247, 2–9. doi: 10.1016/j.geomorph.2015.05.028
Amin, C., Priyono, P., Jauhari, A., Priyana, Y., Priyono, K. D., & Cholil, M. (2017). Management of an underground river to overcome water scarcity in the Gunung Sewu Karst Area, Indonesia. Forum Geografi, 31(1), 176–183. doi: 10.23917/forgeo.v31i1.4502
Cao, Jian-hua, Wu, X., Huang, F., Hu, B., Groves, C., Yang, H., & Zhang, C. (2018). Global significance of the carbon cycle in the karst dynamic system: Evidence from geological and ecological processes. China Geology, 1(1), 17–27. doi: 10.31035/cg2018004
Cao, Jianhua, Hu, B., Groves, C., Huang, F., Yang, H., & Zhang, C. (2016). Karst dynamic system and the carbon cycle. Zeitschrift Für Geomorphologie, Supplementary Issues, 60(2), 35–55. doi: 10.1127/zfg_suppl/2016/00304
Cheng, Z. (2011). Carbonate rock dissolution rates in different landuses and their. Chinese Science Bulletin, 56(35), 3759–3765. doi: 10.1007/s11434-011-4404-4
Danardono, D., Haryono, E., & Widyastuti, M. (2019). The nature of carbon flux in various ecosystem types in the Biduk-Biduk Karst Region, Berau District, East Kalimantan. E3S Web Conf., 76, 1–7. doi: 10.1051/e3sconf/20197604005
Danardono, D., Putra, E. B. D., Haryono, E., Nurjani, E., & Sunariya, M. I. T. (2018). Speleoclimate monitoring to assess cave tourism capacity in Gelatik Cave, Gunungsewu Geopark, Indonesia. Forum Geografi, 32(2), 181–194. doi: 10.23917/forgeo.v32i2.6958
Daoxian, Y., & Cai, G. (1988). Karst Environmental Science. Chongqing: Chongqing Science and Technology Publishing
Djamal, B., Sudana, D., Soetrisno, Baharuddin, & Hasan, K. (1995). Peta Geologi Lembar Tanjung Mangkalihat, Kalimantan. Bandung
Englhart, S., Franke, J., Keuck, V., & Siegert, F. (2014). Carbon stock estimation of tropical forests on Borneo, Indonesia, for REDD+. In I. Manakos & M. Braun (Eds.), Land Use and Land Cover Mapping in Europe: Practices & Trends (pp. 411–427). doi: 10.1007/978-94-007-7969-3_24
Ford, D. C., & Williams, P. W. (2007). Karst Hydrogeology and Geomorphology. Chicester: John Wiley and Sons Inc
Gabrovšek, F. (2009). On concepts and methods for the estimation of dissolutional denudation rates in karst areas. Geomorphology, 106(1), 9–14. doi: 10.1016/j.geomorph.2008.09.008
Haryono, E. (2011, January 11). Atmospheric carbon dioxide sequestrationtrough karst denudation processes estimated from Indonesian karst region. 203–207. Asian Trans-Disciplinary Karst Conference
Haryono, E., Danardono, D., Mulatsih, S., Putro, S. T., & Adji, T. N. (2016a). The nature of carbon flux in Gunungsewu Karst, Java-Indonesia. Acta Carsologica, 45(2). doi: 10.3986/ac.v45i2.4541
Haryono, E., Danardono, D., Mulatsih, S., Putro, S. T., & Adji, T. N. (2016b). The nature of carbon flux in Gunungsewu Karst, Java, Indonesia. Acta Carsologica, 45(1), 173–185
Hertel, D., Moser, G., Culmsee, H., Erasmi, S., Horna, V., Schuldt, B., & Leuschner, C. (2009). Forest ecology and management below- and above-ground biomass and net primary production in a paleotropical natural forest ( Sulawesi , Indonesia ) as compared to neotropical forests. Forest Ecology and Management, 258(9), 1904–1912. doi: 10.1016/j.foreco.2009.07.019
International Energy Agency. (2018). Emissions Factors (2018). France: International Energy Agency
IPCC. (2013). Climate Change 2013: The Physical Science Basis: Working Group 1 Contribution to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. New York: Cambridge University Press
Jiang, Y. (2013). The contribution of human activities to dissolved inorganic carbon fluxes in a karst underground river system: Evidence from major elements and δ13CDIC in Nandong, Southwest China. Journal of Contaminant Hydrology, 152, 1–11. doi: 10.1016/j.jconhyd.2013.05.010
Krklec, K., Domínguez-Villar, D., Carrasco, R. M., & Pedraza, J. (2016). Current denudation rates in dolostone karst from central Spain: Implications for the formation of unroofed caves. Geomorphology, 264, 1–11. doi: 10.1016/j.geomorph.2016.04.007
Liu, Z, & Zhao, J. (2000). Contribution of carbonate rock weathering to the atmospheric CO2 sink. Environmental Geology, 39(9), 1053–1058. doi: 10.1007/s002549900072
Liu, Zaihua, He, S. Y., Yuan, D. X., & Zhao, J. B. (1998). The CO2 regime of soil profile and its drive to dissolution. Hydrology and Engineering Geology, 25, 42–45
Pan, Y., Birdsey, R. A., Fang, J., Houghton, R., Kauppi, P. E., Kurz, W. A., … Hayes, D. (2011). A large and persistent carbon sink in the world’s forests. Science, 333(6045), 988–993. doi: 10.1126/science.1201609
Plan, L. (2005). Factors controlling carbonate dissolution rates quantified in a field test in the Austrian alps. Geomorphology, 68(3), 201–212. doi: 10.1016/j.geomorph.2004.11.014
Rutishauser, E., Noor’an, F., Laumonier, Y., Halperin, J., Rufi’ie, Hergoualc’h, K., & Verchot, L. (2013). Generic allometric models including height best estimate forest biomass and carbon stocks in Indonesia. Forest Ecology and Management, 307, 219–225. doi: 10.1016/j.foreco.2013.07.013
Saner, P., Loh, Y. Y., Ong, R. C., & Hector, A. (2012). Carbon stocks and fluxes in tropical lowland dipterocarp rainforests in Sabah , Malaysian Borneo. 7(1). doi: 10.1371/journal.pone.0029642
Song, X., Gao, Y., Wen, X., Guo, D., Yu, G., He, N., & Zhang, J. (2017). Carbon sequestration potential and its eco-service function in the karst area, China. Journal of Geographical Sciences, 27(8), 967–980. doi: 10.1007/s11442-017-1415-3
Srijono, S., & Nadia, N. (2013). Urang Cave Karst environmental development as tourism object. Forum Geografi, 27(2), 99. doi: 10.23917/forgeo.v27i2.2369
Urushibara-Yoshino, K., Miotke, F.-D., Kashima, N., Enomoto, H., Kuramoto, T., Kina, H., … Higa, M. (1999). Solution rate of limestone in Japan. Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy, 24(10), 899–903. doi: 10.1016/S1464-1895(99)00133-7
Yu, Y., Li, J., Zhou, Z., Zeng, L., & Zhang, C. (2020). Estimation of the value of ecosystem carbon sequestration services under different scenarios in the Central China ( the Qinling-Daba Mountain Area ). Sustainability, 12(337), 1–18
Zhang, C. (2011). Carbonate rock dissolution rates in different landuses and their carbon sink effect. Chinese Science Bulletin, 56(35), 3759–3765. doi: 10.1007/s11434-011-4404-4
Zhongcheng, J., & Daoxian, Y. (1999). CO2 source-sink in karst processes in karst areas of China. International Union of Geological Sciences, 22(1), 33–35. doi: 10.18814/epiiugs/1999/v22i1/005

Last update:

No citation recorded.

Last update:

No citation recorded.

This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License.

As an article writer, the author has the right to use their articles for various purposes, including use by institutions that employ authors or institutions that provide funding for research. Author rights are granted without special permission.

Author who publishes a paper at JWL has the broad right to use their work for teaching and scientific purposes without the need to ask permission, including: used for (i) teaching in the author's class or institution, (ii) presentation at meetings or conferences and distributing copies to participants ; (iii) training conducted by the author or author's institution; (iv) distribution to colleagues for research use; (v) use in the compilation of subsequent authors' works; (vi) inclusion in a thesis or dissertation; (vi) reuse of part of the article in another work (with citation); (vii) preparation of derivative works (with citation); (viii) voluntary posting on open websites operated by authors or author institutions for scientific purposes (follow the CC BY-NC-SA 4.0 License).

Authors and readers can copy and redistribute material in any media or format, and mix, modify, and build material for any purpose but they must provide appropriate credit (provide article citation or content), providing links to the license, and indicate if there are changes.

The authors submitting a manuscript do so on the understanding that if accepted for publication, copyright of the article shall be assigned to Jurnal Wilayah dan Lingkungan (JWL). Copyright encompasses rights to reproduce and deliver the article in all form and media, including reprints, photographs, microfilms and any other similar reproductions, as well as translations.

Reproduce any part of this journal, its storage in the database or its transmission by all forms or media is permitted does not need for written permission from JWL. However, it should be cited as an honor in academic manners

JWL and the Department of Urban and Regional Planning of Diponegoro University and the Editor make every effort to ensure that there are no data, opinions, or false or misleading statements published in JWL. However, the content of the article is the sole and exclusive responsibility of each author.

The Copyright Transfer Form can be downloaded here: [Copyright Transfer Form - Indonesian] [Copyright Transfer Form - English]. The copyright form should be signed originally and send to the Editor in the form of printed letters, scanned documents sent via email or fax.