Effects of spatial variability in vegetation phenology, climate, landcover, biodiversity, topography, and soil property on soil respiration across a coastal ecosystem

被引:6
作者
He, Yinan [1 ]
Bond-Lamberty, Ben [2 ]
Myers-Pigg, Allison N. [3 ,4 ]
Newcomer, Michelle E. [1 ]
Ladau, Joshua [5 ]
Holmquist, James R. [6 ]
Brown, James B. [5 ]
Falco, Nicola [1 ]
机构
[1] Lawrence Berkeley Natl Lab, Earth & Environm Sci Area, 1 Cyclotron Rd, Berkeley, CA 94720 USA
[2] Pacific Northwest Natl Lab, Joint Global Change Res Inst, College Pk, MD 20740 USA
[3] Pacific Northwest Natl Lab, Marine & Coastal Res Lab, Sequim, WA 98382 USA
[4] Univ Toledo, Dept Environm Sci, Toledo, OH 43606 USA
[5] Lawrence Berkeley Natl Lab, Computat Biosci Grp, 1 Cyclotron Rd, Berkeley, CA 94720 USA
[6] Smithsonian Environm Res Ctr, 647 Contees Wharf Rd, Edgewater, MD 21037 USA
关键词
Remote sensing; Harmonized Landsat Sentinel-2; Hierarchical Agglomerative Clustering (HAC); Post hoc hypothesis test; Random Forest (RF); SHapley Additive exPlanations (SHAP); ORGANIC-MATTER MINERALIZATION; TEMPERATURE SENSITIVITY; LAND-USE; SUBSTRATE AVAILABILITY; MICROBIAL ACTIVITY; CARBON DYNAMICS; WETLAND SOILS; WATER; SEDIMENT; CO2;
D O I
10.1016/j.heliyon.2024.e30470
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Coastal terrestrial -aquatic interfaces (TAIs) are crucial contributors to global biogeochemical cycles and carbon exchange. The soil carbon dioxide (CO 2 ) efflux in these transition zones is however poorly understood due to the high spatiotemporal dynamics of TAIs, as various subecosystems in this region are compressed and expanded by complex influences of tides, changes in river levels, climate, and land use. We focus on the Chesapeake Bay region to (i) investigate the spatial heterogeneity of the coastal ecosystem and identify spatial zones with similar environmental characteristics based on the spatial data layers, including vegetation phenology, climate, landcover, diversity, topography, soil property, and relative tidal elevation; (ii) understand the primary driving factors affecting soil respiration within sub -ecosystems of the coastal ecosystem. Specifically, we employed hierarchical clustering analysis to identify spatial regions with distinct environmental characteristics, followed by the determination of main driving factors using Random Forest regression and SHapley Additive exPlanations. Maximum and minimum temperature are the main drivers common to all sub -ecosystems, while each region also has additional unique major drivers that differentiate them from one another. Precipitation exerts an influence on vegetated lands, while soil pH value holds importance specifically in forested lands. In croplands characterized by high clay content and low sand content, the significant role is attributed to bulk density. Wetlands demonstrate the importance of both elevation and sand content, with clay content being more relevant in non -inundated wetlands than in inundated wetlands. The topographic wetness index significantly contributes to the mixed vegetation areas, including shrub, grass, pasture, and forest. Additionally, our research reveals that dense vegetation land covers and urban/developed areas exhibit distinct soil property drivers. Overall, our research demonstrates an efficient method of employing various open -source remote sensing and GIS datasets to comprehend the spatial variability and soil respiration mechanisms in coastal TAI. There is no one -size -fits -all approach to modeling carbon fluxes released by soil respiration in coastal TAIs, and our study highlights the importance of further research and monitoring practices to improve our understanding of carbon dynamics and promote the sustainable management of coastal TAIs.
引用
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页数:17
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