scholarly journals Towards spatial assessment of carbon sequestration in peatlands: spectroscopy based estimation of fractional cover of three plant functional types

2009 ◽  
Vol 6 (2) ◽  
pp. 275-284 ◽  
Author(s):  
G. Schaepman-Strub ◽  
J. Limpens ◽  
M. Menken ◽  
H. M. Bartholomeus ◽  
M. E. Schaepman

Abstract. Peatlands accumulated large carbon (C) stocks as peat in historical times. Currently however, many peatlands are on the verge of becoming sources with their C sequestration function becoming sensitive to environmental changes such as increases in temperature, decreasing water table and enhanced nitrogen deposition. Long term changes in vegetation composition are both, a consequence and indicator of future changes in C sequestration. Spatial continuous accurate assessment of the vegetation composition is a current challenge in keeping a close watch on peatland vegetation changes. In this study we quantified the fractional cover of three major plant functional types (PFTs; Sphagnum mosses, graminoids, and ericoid shrubs) in peatlands, using field spectroscopy reflectance measurements (400–2400 nm) on 25 plots differing in PFT cover. The data was validated using point intercept methodology on the same plots. Our results showed that the detection of open Sphagnum versus Sphagnumcovered by vascular plants (shrubs and graminoids) is feasible with an R2 of 0.81. On the other hand, the partitioning of the vascular plant fraction into shrubs and graminoids revealed lower correlations of R2 of 0.54 and 0.57, respectively. This study was based on a dataset where the reflectance of all main PFTs and their pure components within the peatland was measured at local spatial scales. Spectrally measured species or plant community abundances can further be used to bridge scaling gaps up to canopy scale, ultimately allowing upscaling of the C balance of peatlands to the ecosystem level.

2008 ◽  
Vol 5 (2) ◽  
pp. 1293-1317 ◽  
Author(s):  
G. Schaepman-Strub ◽  
J. Limpens ◽  
M. Menken ◽  
H. M. Bartholomeus ◽  
M. E. Schaepman

Abstract. Peatlands accumulated large carbon stocks as peat in historical times. Currently however, many peatlands are on the verge of becoming sources with their carbon sequestration function becoming sensitive to environmental changes such as increases in temperature, decreasing water table and enhanced nitrogen deposition. Long term changes in vegetation composition are both, a consequence and indicator of future changes in carbon sequestration. Spatial continuous accurate assessment of the vegetation composition is a current challenge in keeping a close watch on peatland vegetation changes. In this study we quantified the fractional cover of three major plant functional types (Sphagnum mosses, graminoids, and shrubs) in peatlands, using field spectroscopy reflectance measurements (400–2400 nm) on 25 plots differing in plant functional type cover. The data was validated using point intercept methodology on the same plots. Our results showed that the detection of open Sphagnum versus Sphagnum covered by vascular plants (shrubs and graminoids) is feasible with an R2 of 0.81. On the other hand, the partitioning of the vascular plant fraction into shrubs and graminoids revealed lower correlations of R2 of 0.54 and 0.57, respectively. This study was based on a dataset where the reflectance of all main plant functional types and their pure components within the peatland was measured at local spatial scales. Spectrally measured species or plant community abundances can further be used to bridge scaling gaps up to canopy scale, ultimately allowing upscaling of the C balance of peatlands to the ecosystem level.


Trees ◽  
1999 ◽  
Vol 14 (2) ◽  
pp. 72 ◽  
Author(s):  
G. Jiang ◽  
Haiping Tang ◽  
M. Yu ◽  
Ming Dong ◽  
Xinshi Zhang

2015 ◽  
Vol 12 (14) ◽  
pp. 4373-4383 ◽  
Author(s):  
Z. Luo ◽  
E. Wang ◽  
H. Zheng ◽  
J. A. Baldock ◽  
O. J. Sun ◽  
...  

Abstract. Soil carbon (C) models are important tools for understanding soil C balance and projecting C stocks in terrestrial ecosystems, particularly under global change. The initialization and/or parameterization of soil C models can vary among studies even when the same model and data set are used, causing potential uncertainties in projections. Although a few studies have assessed such uncertainties, it is yet unclear what these uncertainties are correlated with and how they change across varying environmental and management conditions. Here, applying a process-based biogeochemical model to 90 individual field experiments (ranging from 5 to 82 years of experimental duration) across the Australian cereal-growing regions, we demonstrated that well-designed optimization procedures enabled the model to accurately simulate changes in measured C stocks, but did not guarantee convergent forward projections (100 years). Major causes of the projection uncertainty were due to insufficient understanding of how microbial processes and soil C pool change to modulate C turnover. For a given site, the uncertainty significantly increased with the magnitude of future C input and years of the projection. Across sites, the uncertainty correlated positively with temperature but negatively with rainfall. On average, a 331 % uncertainty in projected C sequestration ability can be inferred in Australian agricultural soils. This uncertainty would increase further if projections were made for future warming and drying conditions. Future improvement in soil C modelling should focus on how the microbial community and its C use efficiency change in response to environmental changes, and better conceptualization of heterogeneous soil C pools and the C transformation among those pools.


2020 ◽  
Author(s):  
Anna V. Roser

Drylands cover 41% of the global land surface and provide ecosystem services to 38% of the world’s population. Dryland ecosystems have already been degraded or threatened by the increased rates of wildfire and invasive annual grasses, as well as changes in precipitation patterns. We cannot protect, mitigate, or restore drylands without comprehensive vegetation surveys. To understand ecosystem processes, we need to know the composition of vegetation at the patch and plant scales. Field observations are limited in coverage, and are expensive and time intensive. Data from Unmanned Aircraft Systems (UAS) will fill the niche between field data and medium scale remotely sensed data, and support the potential for upscaling. UAS-based remote sensing will also help extend the spatiotemporal scope of field surveys, improving efficiency and effectiveness. This study aims to test UAS methods to estimate two important vegetation metrics (1) fractional photosynthetic cover and (2) fractional cover of plant functional types. For both objectives, a series of surveys were conducted using fine-scale spatial resolution (1-4 cm pixel-1) multispectral UAS data collected in Reynolds Creek Experimental Watershed in Southwestern Idaho, USA. Data were collected at three sites along an elevation and precipitation gradient. Each site is characterized by a different type of sagebrush: Wyoming Big Sage, Low sage, and Mountain big sage. The first study in this thesis tests multiple vegetation indices at each site to assess their accuracy in modeling photosynthetic cover. We found the Modified Soil Adjusted Vegetation index (MSAVI) had the highest accuracy when modeling photosynthetic cover at each site (62-93%). The modeled photosynthetic cover was compared to field data consisting of point frame plots (n = 30) at each site. Correlations between field and UAS-derived cover estimates showed significant positive relationships at the Low Sage (r = 0.75, pr = 0.55, p = 0.002), but not at Wyoming Big Sage (r = 0.10, p = 0.61). These results demonstrate methods to estimate photosynthetic cover at fine scales in three types of sagebrush using UAS imagery. Additionally, these results suggest that UAS surveys has high correlation with field measurements at mid and high elevation sagebrush sites, but more studies are needed in low elevation sites to understand the potential of integrating UAS and field observations of photosynthetic cover. Our second study quantified fractional cover of plant functional types in the same three sagebrush sites listed above. First, we tested Object-Based Image Analysis (OBIA) for classification of UAS surveys into plant functional types. We assessed the accuracy of the maps using confusion matrices; overall classification accuracies were strong: Wyoming Big Sage (70%), Low Sage (73%), and Mountain Big Sage (78%). The classified maps of plant functional types were compared to data from field plots (n = 30) at each site. We found significant positive correlations for shrubs (r = 0.58; 0.83), forbs (r = 0.39; 0.94), and bare ground (r = 0.61; 0.70) at our Low Sage and Mountain Big Sage. However we did not find significant relationships for the gramminoid class at any site (r = 0.18; 0.3; 0.32). Second, we tested the application of OBIA to sum shrub abundance from UAS imagery. Abundance data from field plots (n= 24 per site) were tested for agreement with UAS imagery. We found no correlation at any site with field observations at the 10m2 scale (r = -0.22; 0.12; 0.26). Overall, we were able to calculate percent cover for large-unit plant functional types, such as shrubs, trees, and some forbs. Accuracy for gramminoid classification was low due to small plant size, confounding soil reflectance, and grasses that grew beneath shrub canopies. This research demonstrates that UAS methods can be used to estimate photosynthetic cover and map plant functional types. Using UAS surveys also increased coverage and sampling density of data when compared to traditional field observations. These findings help land managers, restoration experts, and other researchers who monitor, manage, and protect dryland ecosystems by demonstrating an accurate and less expensive approach to collecting ecosystem data.


Forests ◽  
2021 ◽  
Vol 12 (8) ◽  
pp. 1007
Author(s):  
Kechao Huang ◽  
Quan Wang ◽  
Dennis Otieno

Subtropical mixed forest ecosystems are experiencing dramatic changes in precipitation and different plant functional types growing here are expected to respond differently. This study aims to unravel the water use patterns of different plant functional types and their responses to environmental changes in a typical subtropical mixed forest in southern China. Diurnal and seasonal sap flux densities of evergreen broad-leaved trees (EBL), deciduous broad-leaved trees (DBL), and conifers (CON), as well as environmental variables, were recorded simultaneously from May 2016 to March 2019. The results showed that the sap flux density of EBL was significantly higher than those of CON and DBL in all seasons, irrespective of dry or wet seasons. Path analysis revealed that seasonal differences in sap flux density were mainly due to variations in photosynthetic photon flux density (PPFD). At saturating PPFD, changes in sap flux density during the day were in response to vapor pressure deficit (VPD). Regression analyses showed that sap flux density increased logarithmically with PPFD, irrespective of functional type. The hysteresis loops of sap flux density and VPD were different among different plant functional types in wet and dry seasons. Our results demonstrated converging response patterns to environmental variables among the three plant functional types considered in this study. Our findings contribute to a better understanding of the water use strategies of different plant functional types in subtropical mixed forests.


2015 ◽  
Vol 12 (12) ◽  
pp. 3805-3818 ◽  
Author(s):  
M. F. Adame ◽  
N. S. Santini ◽  
C. Tovilla ◽  
A. Vázquez-Lule ◽  
L. Castro ◽  
...  

Abstract. Riverine wetlands are created and transformed by geomorphological processes that determine their vegetation composition, primary production and soil accretion, all of which are likely to influence C stocks. Here, we compared ecosystem C stocks (trees, soil and downed wood) and soil N stocks of different types of riverine wetlands (marsh, peat swamp forest and mangroves) whose distribution spans from an environment dominated by river forces to an estuarine environment dominated by coastal processes. We also estimated soil C sequestration rates of mangroves on the basis of soil C accumulation. We predicted that C stocks in mangroves and peat swamps would be larger than marshes, and that C, N stocks and C sequestration rates would be larger in the upper compared to the lower estuary. Mean C stocks in mangroves and peat swamps (784.5 ± 73.5 and 722.2 ± 63.6 MgC ha−1, respectively) were higher than those of marshes (336.5 ± 38.3 MgC ha−1). Soil C and N stocks of mangroves were highest in the upper estuary and decreased towards the lower estuary. C stock variability within mangroves was much lower in the upper estuary (range 744–912 MgC ha−1) compared to the intermediate and lower estuary (range 537–1115 MgC ha−1) probably as a result of a highly dynamic coastline. Soil C sequestration values were 1.3 ± 0.2 MgC ha−1 yr−1 and were similar across sites. Estimations of C stocks within large areas need to include spatial variability related to vegetation composition and geomorphological setting to accurately reflect variability within riverine wetlands.


2016 ◽  
Vol 2016 ◽  
pp. 1-11 ◽  
Author(s):  
Alexander B. Novakovskiy ◽  
Svetlana P. Maslova ◽  
Igor V. Dalke ◽  
Yuriy A. Dubrovskiy

Morphological and physiological parameters of 76 vascular plant species typical for Northern Europe were analyzed using Grime’s classification.Cspecies (competitors) have high levels of canopy height, leaf dry weight, and maximal lateral spread.Rspecies (ruderal) have low leaf dry weight, longer flowering period, high rate of photosynthetic capacity and respiration, and high nitrogen content in the leaves. Stress-tolerant (S) species prevailing in habitats with limited resources are small and have low rate of photosynthetic activity and respiration. Principal component analysis (PCA) ordination showed a clear separation of species of different plant functional types according to their morphological and physiological parameters. The first PCA axis showed close relationship with the rate of respiration and photosynthetic activity and allowed us to differentiateSfromRspecies. The second PCA axis correlated with morphological parameters associated with the size of plants and allowed us to differentiateCspecies fromSandRspecies. Using PCA ordination, we developed a model that determines plant functional types in Northern Europe and analyzed plant functional types of several species that are not presented in Grime’s classification. The proposed model has higher accuracy (84%) compared to similar models designed for other climatic zones.


2015 ◽  
Vol 103 (4) ◽  
pp. 925-934 ◽  
Author(s):  
Bjorn J. M. Robroek ◽  
Vincent E. J. Jassey ◽  
Martine A. R. Kox ◽  
Roeland L. Berendsen ◽  
Robert T. E. Mills ◽  
...  

2015 ◽  
Vol 407 (1-2) ◽  
pp. 135-143 ◽  
Author(s):  
Bjorn J. M. Robroek ◽  
Remy J. H. Albrecht ◽  
Samuel Hamard ◽  
Adrian Pulgarin ◽  
Luca Bragazza ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document