Accumulation of SOC in relatively undisturbed tropical mountain foothills under climate change scenarios: The case of Uluguru Mountain, Tanzania
Soil nutrients form an important part of agro-ecosystems in various landscapes, including mountainous areas. Most foothills in tropical mountains are heterogeneous in terms of the accumulation of soil nutrients due climatic location and ecological endowments. Since most mountain foothills have poten...
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description | Soil nutrients form an important part of agro-ecosystems in various landscapes, including mountainous areas. Most foothills in tropical mountains are heterogeneous in terms of the accumulation of soil nutrients due climatic location and ecological endowments. Since most mountain foothills have potential for the provision of environmental services, it is imperative to assess the salient soil nutrients including carbon in order to determine the amount. This study assessed the accumulation of soil organic carbon (SOC) in the relatively undisturbed foothills of Uluguru Mountains whose geology indicates that they were formed during cretaceous age (i.e. ≈50 million years ago). The study also determined the trends of rainfall and temperature because these elements of climate have important influence on carbon accumulation. In conducting this study, we sampled Kiroka Village (in Kiroka Ward) because it is found at the foothills of the Uluguru Mountain and most of its parts are relatively undisturbed. In this place, sixteen soil sampling points were established within one hectare and these points involved two soil depths (i.e. 0-20 cm and 20-40 cm) and two locations (i.e. lowland and upland). The Walkley–Black Method was used for SOC analysis while Mann–Kendall Test was employed for climate data analysis. The results exhibit that there have been significant variations in SOC accumulation under the two soil depths and locations. In the lowland areas, SOC was 1.1 and 0.43 MgC ha
−1
for the depths 0–20 cm and 20–40, respectively. Besides, in upland areas, SOC was 0.38 and 0.31 MgC ha
−1
for the depths 0–20 cm and 20–40, respectively. Most cereal crops require a considerable amount of SOC in the soil that ranges between 0.5 and 2 MgC ha
−1
. Additionally, the mean annual rainfall and temperature patterns from 1980 to 2020 declined and intensified at R
2
= 0.15 and 0.19, respectively. Therefore, these results inform environmental experts, climate practitioners and other relevant stakeholders to endorse suitable and sustainable environmental management methods in the mountainous areas. |
doi_str_mv | 10.1007/s12517-023-11574-z |
format | Article |
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−1
for the depths 0–20 cm and 20–40, respectively. Besides, in upland areas, SOC was 0.38 and 0.31 MgC ha
−1
for the depths 0–20 cm and 20–40, respectively. Most cereal crops require a considerable amount of SOC in the soil that ranges between 0.5 and 2 MgC ha
−1
. Additionally, the mean annual rainfall and temperature patterns from 1980 to 2020 declined and intensified at R
2
= 0.15 and 0.19, respectively. Therefore, these results inform environmental experts, climate practitioners and other relevant stakeholders to endorse suitable and sustainable environmental management methods in the mountainous areas.</description><identifier>ISSN: 1866-7511</identifier><identifier>EISSN: 1866-7538</identifier><identifier>DOI: 10.1007/s12517-023-11574-z</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Accumulation ; Agricultural ecosystems ; Annual rainfall ; Carbon ; Cereal crops ; Climate change ; Climatic data ; Cretaceous ; Data analysis ; Depth ; Earth and Environmental Science ; Earth science ; Earth Sciences ; Environmental management ; Environmental services ; Foothills ; Geology ; Management methods ; Mountain regions ; Mountainous areas ; Mountains ; Nutrients ; Organic carbon ; Organic soils ; Original Paper ; Precipitation ; Soil ; Soil depth ; Soil nutrients ; Soil sampling ; Sustainability management ; Temperature</subject><ispartof>Arabian journal of geosciences, 2023, Vol.16 (7), Article 445</ispartof><rights>Saudi Society for Geosciences and Springer Nature Switzerland AG 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c115z-65130d946f8379ca9e0563aeaa39d361e0c98ed77281e8df29f005cd5d03abc73</cites><orcidid>0000-0002-1626-3724</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12517-023-11574-z$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12517-023-11574-z$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27915,27916,41479,42548,51310</link.rule.ids></links><search><creatorcontrib>Mkonda, Msafiri Y.</creatorcontrib><creatorcontrib>Minja, Gileard S.</creatorcontrib><creatorcontrib>Ligate, Elly J.</creatorcontrib><creatorcontrib>Kaganga, Laison S.</creatorcontrib><creatorcontrib>Haule, Tiemo R.</creatorcontrib><creatorcontrib>Msemwa, Ubaya S.</creatorcontrib><title>Accumulation of SOC in relatively undisturbed tropical mountain foothills under climate change scenarios: The case of Uluguru Mountain, Tanzania</title><title>Arabian journal of geosciences</title><addtitle>Arab J Geosci</addtitle><description>Soil nutrients form an important part of agro-ecosystems in various landscapes, including mountainous areas. Most foothills in tropical mountains are heterogeneous in terms of the accumulation of soil nutrients due climatic location and ecological endowments. Since most mountain foothills have potential for the provision of environmental services, it is imperative to assess the salient soil nutrients including carbon in order to determine the amount. This study assessed the accumulation of soil organic carbon (SOC) in the relatively undisturbed foothills of Uluguru Mountains whose geology indicates that they were formed during cretaceous age (i.e. ≈50 million years ago). The study also determined the trends of rainfall and temperature because these elements of climate have important influence on carbon accumulation. In conducting this study, we sampled Kiroka Village (in Kiroka Ward) because it is found at the foothills of the Uluguru Mountain and most of its parts are relatively undisturbed. In this place, sixteen soil sampling points were established within one hectare and these points involved two soil depths (i.e. 0-20 cm and 20-40 cm) and two locations (i.e. lowland and upland). The Walkley–Black Method was used for SOC analysis while Mann–Kendall Test was employed for climate data analysis. The results exhibit that there have been significant variations in SOC accumulation under the two soil depths and locations. In the lowland areas, SOC was 1.1 and 0.43 MgC ha
−1
for the depths 0–20 cm and 20–40, respectively. Besides, in upland areas, SOC was 0.38 and 0.31 MgC ha
−1
for the depths 0–20 cm and 20–40, respectively. Most cereal crops require a considerable amount of SOC in the soil that ranges between 0.5 and 2 MgC ha
−1
. Additionally, the mean annual rainfall and temperature patterns from 1980 to 2020 declined and intensified at R
2
= 0.15 and 0.19, respectively. Therefore, these results inform environmental experts, climate practitioners and other relevant stakeholders to endorse suitable and sustainable environmental management methods in the mountainous areas.</description><subject>Accumulation</subject><subject>Agricultural ecosystems</subject><subject>Annual rainfall</subject><subject>Carbon</subject><subject>Cereal crops</subject><subject>Climate change</subject><subject>Climatic data</subject><subject>Cretaceous</subject><subject>Data analysis</subject><subject>Depth</subject><subject>Earth and Environmental Science</subject><subject>Earth science</subject><subject>Earth Sciences</subject><subject>Environmental management</subject><subject>Environmental services</subject><subject>Foothills</subject><subject>Geology</subject><subject>Management methods</subject><subject>Mountain regions</subject><subject>Mountainous areas</subject><subject>Mountains</subject><subject>Nutrients</subject><subject>Organic carbon</subject><subject>Organic soils</subject><subject>Original Paper</subject><subject>Precipitation</subject><subject>Soil</subject><subject>Soil depth</subject><subject>Soil nutrients</subject><subject>Soil sampling</subject><subject>Sustainability management</subject><subject>Temperature</subject><issn>1866-7511</issn><issn>1866-7538</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNp9kMtKAzEUhoMoWKsv4Crg1tFk0snFXSneoNKF7TqkmUw7ZZrUZCJ0nsJHNmOL7lwlHL7_P5wPgGuM7jBC7D7gvMAsQznJMC7YKOtOwABzSjNWEH76-8f4HFyEsEGIcsT4AHyNtY7b2Ki2dha6Cr7PJrC20Jt-9GmaPYy2rEMb_dKUsPVuV2vVwK2LtlUJrJxr13XThJ4zHuqm3qrWQL1WdmVg0MYqX7vwAOfrNFXB9FsWTVxFH-HbseYWzpXtlK3VJTirVBPM1fEdgsXT43zykk1nz6-T8TTT6cAuowUmqBQjWnHChFbCoIISZZQioiQUG6QFNyVjOceGl1UuKoQKXRYlImqpGRmCm0PvzruPaEIrNy56m1bKnBMsBBW0p_IDpb0LwZtK7ny6z-8lRrI3Lw_mZTIvf8zLLoXIIRQSnCT4v-p_Ut_72YoM</recordid><startdate>2023</startdate><enddate>2023</enddate><creator>Mkonda, Msafiri Y.</creator><creator>Minja, Gileard S.</creator><creator>Ligate, Elly J.</creator><creator>Kaganga, Laison S.</creator><creator>Haule, Tiemo R.</creator><creator>Msemwa, Ubaya S.</creator><general>Springer International Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0002-1626-3724</orcidid></search><sort><creationdate>2023</creationdate><title>Accumulation of SOC in relatively undisturbed tropical mountain foothills under climate change scenarios: The case of Uluguru Mountain, Tanzania</title><author>Mkonda, Msafiri Y. ; Minja, Gileard S. ; Ligate, Elly J. ; Kaganga, Laison S. ; Haule, Tiemo R. ; Msemwa, Ubaya S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c115z-65130d946f8379ca9e0563aeaa39d361e0c98ed77281e8df29f005cd5d03abc73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Accumulation</topic><topic>Agricultural ecosystems</topic><topic>Annual rainfall</topic><topic>Carbon</topic><topic>Cereal crops</topic><topic>Climate change</topic><topic>Climatic data</topic><topic>Cretaceous</topic><topic>Data analysis</topic><topic>Depth</topic><topic>Earth and Environmental Science</topic><topic>Earth science</topic><topic>Earth Sciences</topic><topic>Environmental management</topic><topic>Environmental services</topic><topic>Foothills</topic><topic>Geology</topic><topic>Management methods</topic><topic>Mountain regions</topic><topic>Mountainous areas</topic><topic>Mountains</topic><topic>Nutrients</topic><topic>Organic carbon</topic><topic>Organic soils</topic><topic>Original Paper</topic><topic>Precipitation</topic><topic>Soil</topic><topic>Soil depth</topic><topic>Soil nutrients</topic><topic>Soil sampling</topic><topic>Sustainability management</topic><topic>Temperature</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Mkonda, Msafiri Y.</creatorcontrib><creatorcontrib>Minja, Gileard S.</creatorcontrib><creatorcontrib>Ligate, Elly J.</creatorcontrib><creatorcontrib>Kaganga, Laison S.</creatorcontrib><creatorcontrib>Haule, Tiemo R.</creatorcontrib><creatorcontrib>Msemwa, Ubaya S.</creatorcontrib><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Arabian journal of geosciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Mkonda, Msafiri Y.</au><au>Minja, Gileard S.</au><au>Ligate, Elly J.</au><au>Kaganga, Laison S.</au><au>Haule, Tiemo R.</au><au>Msemwa, Ubaya S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Accumulation of SOC in relatively undisturbed tropical mountain foothills under climate change scenarios: The case of Uluguru Mountain, Tanzania</atitle><jtitle>Arabian journal of geosciences</jtitle><stitle>Arab J Geosci</stitle><date>2023</date><risdate>2023</risdate><volume>16</volume><issue>7</issue><artnum>445</artnum><issn>1866-7511</issn><eissn>1866-7538</eissn><abstract>Soil nutrients form an important part of agro-ecosystems in various landscapes, including mountainous areas. Most foothills in tropical mountains are heterogeneous in terms of the accumulation of soil nutrients due climatic location and ecological endowments. Since most mountain foothills have potential for the provision of environmental services, it is imperative to assess the salient soil nutrients including carbon in order to determine the amount. This study assessed the accumulation of soil organic carbon (SOC) in the relatively undisturbed foothills of Uluguru Mountains whose geology indicates that they were formed during cretaceous age (i.e. ≈50 million years ago). The study also determined the trends of rainfall and temperature because these elements of climate have important influence on carbon accumulation. In conducting this study, we sampled Kiroka Village (in Kiroka Ward) because it is found at the foothills of the Uluguru Mountain and most of its parts are relatively undisturbed. In this place, sixteen soil sampling points were established within one hectare and these points involved two soil depths (i.e. 0-20 cm and 20-40 cm) and two locations (i.e. lowland and upland). The Walkley–Black Method was used for SOC analysis while Mann–Kendall Test was employed for climate data analysis. The results exhibit that there have been significant variations in SOC accumulation under the two soil depths and locations. In the lowland areas, SOC was 1.1 and 0.43 MgC ha
−1
for the depths 0–20 cm and 20–40, respectively. Besides, in upland areas, SOC was 0.38 and 0.31 MgC ha
−1
for the depths 0–20 cm and 20–40, respectively. Most cereal crops require a considerable amount of SOC in the soil that ranges between 0.5 and 2 MgC ha
−1
. Additionally, the mean annual rainfall and temperature patterns from 1980 to 2020 declined and intensified at R
2
= 0.15 and 0.19, respectively. Therefore, these results inform environmental experts, climate practitioners and other relevant stakeholders to endorse suitable and sustainable environmental management methods in the mountainous areas.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><doi>10.1007/s12517-023-11574-z</doi><orcidid>https://orcid.org/0000-0002-1626-3724</orcidid></addata></record> |
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subjects | Accumulation Agricultural ecosystems Annual rainfall Carbon Cereal crops Climate change Climatic data Cretaceous Data analysis Depth Earth and Environmental Science Earth science Earth Sciences Environmental management Environmental services Foothills Geology Management methods Mountain regions Mountainous areas Mountains Nutrients Organic carbon Organic soils Original Paper Precipitation Soil Soil depth Soil nutrients Soil sampling Sustainability management Temperature |
title | Accumulation of SOC in relatively undisturbed tropical mountain foothills under climate change scenarios: The case of Uluguru Mountain, Tanzania |
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