Soil Type, Topography, and Land Use Interact to Control the Response of Soil Respiration to Climate Variation

Abstract

The effects of soil and topography on the responses of soil respiration (Rs) to climatic variables must be investigated in the southeastern mountainous areas of China due to the rapid land-use change from forest to agriculture. In this study, we investigated the response of Rs to soil temperature (ST), precipitation over the previous seven days (AP7), and soil water content (SWC) across two hillslopes that had different land uses: a tea garden (TG) and a bamboo forest (BF). Meanwhile, the roles of soil properties including soil clay content and total nitrogen (TN), and topography including elevation, profile curvature (PRC), and slope on the different responses of Rs to these climatic variables were investigated. Results showed that mean Rs on the BF hillslope (2.21 umol C m−2 s−1) was 1.71 times of that on the TG hillslope (1.29 umol C m−2 s−1). Soil clay content, elevation, and PRC had negative correlations (p < 0.05) with spatial variation of Rs, and ST was positively correlated (p < 0.01) with temporal variation of Rs on both hillslopes. Across both hillslopes ST explained 33%–73% and AP7 explained 24%–38% of the temporal variations in Rs. The mean temperature sensitivities (Q10s) of Rs were 2.02 and 3.22, respectively, on the TG and BF hillslopes. The Q10 was positively correlated (p < 0.05) with the temporal mean of SWC and TN, and negatively correlated (p < 0.05) with clay and slope. The mean AP7 sensitivities (a concept similar to Q10) were greatly affected by clay and PRC. When Rs was normalized to that at 10 °C, power or quadratic relationships between Rs and SWC were observed in different sites, and the SWC explained 12%–32% of the temporal variation in Rs. When ST and SWC were integrated and considered, improved explanations (45%–81%) were achieved for the Rs temporal variation. In addition, clay and elevation had vital influences on the responses of Rs to SWC. These results highlight the influences of soil, topographic features, and land use on the spatial variations of the Rs, as well as on the responses of Rs to different climatic variables, which will supplement the understanding of controlling mechanisms of Rs on tea and bamboo land-use types in Southeastern China.

Global patterns and edaphic-climatic controls of soil carbon decomposition kinetics predicted from incubation experiments

“…As a key proxy of soil physical properties, soil texture 54 , especially clay content, exhibited strong influence on M3-k1 ref and M3-k2 ref . Higher soil respiration was generally measured from finer-textured soil with a higher proportion of clay within a specific threshold, where microbial activity was higher as a result of greater soil water holding capacity and nutrient availability 55 – 57 . However, a higher clay content means a potentially higher proportion of mineral-associated organic matter which could be prevented from microbial utilization, leading to the reduction of SOM decomposition rates 58 , 59 .…”

Relationship between Rural Settlements’ Plant Communities and Environmental Factors in Hilly Area of Southeast China

“…Several studies were conducted to explore the influencing factors, including environmental factors such as climate, soil, and topography, and their correlation mechanisms to the patterns of plant community distributions [16]. Altitudes and slope aspects have a significant impact on the growth of trees [27,28], and topographic factors affect the growth and diversity of plants according to different soil properties [29]. Moreover, soil type, topography and spatial scale have a significant impact on the collective distribution of subtropical forest communities [30].…”

Uso e cobertura do solo na bacia hidrográfica do rio Doce (MG/ES): inter-relações para a governança

“…Podem, ainda, alterar a distribuição espacial do teor de água do solo, da concentração de gases no solo, de nutrientes e de temperatura, resultando na heterogeneidade espacial. Considerar o efeito dessas variáveis espaciais nas respostas locais, ao longo do tempo, traz uma oportunidade significativa de aprimorar a capacidade de explicar e prever as respostas ambientais às mudanças ao uso do solo e do clima (APAN, PETERSON, 1998;SILVA et al, 2007;TURNER, RUSCHER, 1988;WANG et al, 2019).…”

“…A literatura relacionada ao tema mostra inúmeras iniciativas realizadas para o mapeamento, o monitoramento e a modelagem do uso e cobertura do solo, em escalas locais, regionais e globais, sendo o seu uso crescente . No entanto, a resposta dos padrões de uso aos processos biofísicos em uma escala de bacia hidrográfica precisa ainda de maior compreensão (WANG, 2019). A bacia hidrográfica do rio Doce (BHRD) apresenta grande importância nacional, mas também diversos desafios para a sua gestão.…”