Ecosystem‐scale carbon allocation among different land uses: implications for carbon stocks in the Yellow River Delta

Abstract

The reclamation area of the Chinese Yellow River Delta (YRD) has experienced frequent land use changes in recent decades. The consequence of such land use changes on the stocks and allocation of ecosystem-scale carbon is not known. Here, we assessed carbon stocks and allocation of four representative land uses in the YRD area: (1) purple alfalfa (LAL), (2) reed and Aeluropus littoralis (RAE), (3) cotton (ECO), and (4) Chinese tamarisk (CTA). The results showed that the overall carbon stocks, and carbon stocks of aboveground, litter, roots, and soil were notably different among different land uses. The native CTA land had the largest overall carbon stock (belowground and aboveground) and had the strongest potential to allocate the carbon to the soil carbon pool (95.72%), followed by the natural grassland (RAE). Alfalfa grassland (LAL) also had a large carbon stock due to its large aboveground biomass, litter, and roots, but the relative allocation proportion of soil carbon stock was lower than that of the other land uses examined. Cotton (ECO) had the lowest soil carbon and total carbon stocks among four land uses. In combining our data on the carbon pool with changes of land use in the YRD area, we argued that land reclamation in the YRD area was likely to turn this area from a carbon sink to carbon source with the release of soil organic carbon. Therefore, cautions should be taken to reduce carbon release, if the reclaimed land be used to plant crops.

Spatiotemporal Variation Characteristics and Dynamic Persistence Analysis of Carbon Sources/Sinks in the Yellow River Basin

“…Most of the upper and middle reaches of the Yellow River basin are located in arid and semiarid areas of China [24], and the ecological environment is very sensitive and fragile [25]. In the context of long-term interference from climate change and high-intensity, largescale human development and construction activities [26], the overall and systematic ecological degradation of the basin is prominent [25]; examples include the decline of natural grassland and wetland functions in the upper reaches [27], the severe soil erosion in the middle reaches [28], the numerous legacy problems in the downstream beaches, and the severe shrinkage of wetland areas in the estuarine delta [29,30]. The carbon balance of the Yellow River basin has a direct bearing on the realization of the "dual carbon" goals in China and has been the focus of much scholarly attention.…”

“…Tian et al [32] analyzed the temporal and spatial change processes of NPP in the Yellow River basin from 1981 to 2020 and its response to meteorological factors. These studies were limited to small areas of the Yellow River basin [29,33] or were focused on vegetation cover, NPP, NDVI, EVI (Enhanced Vegetation Index), etc. [34].…”