{"title":"Temporal–spatial variations of soil respiration and the controlling factors on global scale (1991–2015)","authors":"","doi":"10.1016/j.gexplo.2024.107562","DOIUrl":null,"url":null,"abstract":"<div><p>Temporal–spatial variations of soil respiration and the controlling factors is important for understanding the global carbon cycle process. In this research, the Global Soil Respiration Database (SRDB) and Global Geochemical Baseline (GGB) dataset were used, temporal–spatial variations of soil respiration from 1991 to 2015 and the controlling factors in soils developed from different soil parent materials were analyzed. We found, for the first time, soil respiration was significantly varied in soils developed from different soil parent materials on a global scale, which was mainly controlled by geochemical indexes such as Al/Si, MnO, CaO and P<sub>2</sub>O<sub>5</sub>. We also found that temporal variations of soil respiration during 1991–2015 in acidic plutonic rocks, acidic volcanic rocks, metamorphic rocks, siliciclastic sedimentary rocks and unconsolidated sediments–developed soils was significantly controlled by temperature, while that of basic plutonic rocks, basic volcanic rocks, intermediate volcanic rocks, mixed sedimentary rocks and carbonate rocks–developed soils was less sensitive to temperature relatively. We conclude that temporal–spatial variations of soil respiration were correlated with soil geochemistry, which mainly depends on the stability difference caused by the bonding between soil organic carbon and soil minerals. The findings may be helpful to understand the temporal–spatial pattern of global soil respiration, moreover reveal the importance of soil geochemistry in influencing soil respiration on global scale.</p></div>","PeriodicalId":16336,"journal":{"name":"Journal of Geochemical Exploration","volume":null,"pages":null},"PeriodicalIF":3.4000,"publicationDate":"2024-08-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geochemical Exploration","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S037567422400178X","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
Temporal–spatial variations of soil respiration and the controlling factors is important for understanding the global carbon cycle process. In this research, the Global Soil Respiration Database (SRDB) and Global Geochemical Baseline (GGB) dataset were used, temporal–spatial variations of soil respiration from 1991 to 2015 and the controlling factors in soils developed from different soil parent materials were analyzed. We found, for the first time, soil respiration was significantly varied in soils developed from different soil parent materials on a global scale, which was mainly controlled by geochemical indexes such as Al/Si, MnO, CaO and P2O5. We also found that temporal variations of soil respiration during 1991–2015 in acidic plutonic rocks, acidic volcanic rocks, metamorphic rocks, siliciclastic sedimentary rocks and unconsolidated sediments–developed soils was significantly controlled by temperature, while that of basic plutonic rocks, basic volcanic rocks, intermediate volcanic rocks, mixed sedimentary rocks and carbonate rocks–developed soils was less sensitive to temperature relatively. We conclude that temporal–spatial variations of soil respiration were correlated with soil geochemistry, which mainly depends on the stability difference caused by the bonding between soil organic carbon and soil minerals. The findings may be helpful to understand the temporal–spatial pattern of global soil respiration, moreover reveal the importance of soil geochemistry in influencing soil respiration on global scale.
期刊介绍:
Journal of Geochemical Exploration is mostly dedicated to publication of original studies in exploration and environmental geochemistry and related topics.
Contributions considered of prevalent interest for the journal include researches based on the application of innovative methods to:
define the genesis and the evolution of mineral deposits including transfer of elements in large-scale mineralized areas.
analyze complex systems at the boundaries between bio-geochemistry, metal transport and mineral accumulation.
evaluate effects of historical mining activities on the surface environment.
trace pollutant sources and define their fate and transport models in the near-surface and surface environments involving solid, fluid and aerial matrices.
assess and quantify natural and technogenic radioactivity in the environment.
determine geochemical anomalies and set baseline reference values using compositional data analysis, multivariate statistics and geo-spatial analysis.
assess the impacts of anthropogenic contamination on ecosystems and human health at local and regional scale to prioritize and classify risks through deterministic and stochastic approaches.
Papers dedicated to the presentation of newly developed methods in analytical geochemistry to be applied in the field or in laboratory are also within the topics of interest for the journal.