five

Seasonal precipitation distribution determines ecosystem CO₂ and H₂O exchange by regulating spring soil water-salt dynamics in a brackish wetland

收藏
Mendeley Data2024-06-29 更新2024-06-29 收录
下载链接:
https://datadryad.org/stash/dataset/doi:10.5061/dryad.pc866t1z3
下载链接
链接失效反馈
官方服务:
资源简介:
# Seasonal precipitation distribution determines ecosystem CO₂ and H₂O exchange by regulating spring soil water-salt dynamics in a brackish wetland [https://doi.org/10.5061/dryad.pc866t1z3](https://doi.org/10.5061/dryad.pc866t1z3) ## Description of the data and file structure Data usage bootstrap: See abiotic factors data at: Huang et al.\_ abiotic factors See biotic factors data at: Huang et al.\_ biotic factors See ecosystem CO₂ and H₂O exchange data at: Huang et al.\_ ecosystem CO₂ and H₂O exchange See structural equation model fitting at: Huang et al.\_ SEM See simulated precipitation at: Huang et al.\_ Precipitation ## DATA-SPECIFIC INFORMATION FOR: Huang et al.\_ abiotic factors 1. Number of variables: 3 2. Number of sheets: 3 3. Number of cases/rows: 6 columns 366 rows/sheet #### Variable List: * EC: soil electrical conductivity ds/m * "Soil electrical conductivity" refers to the ability of ions dissolved in soil solution to conduct current. It is a measure of the soluble salt content of soil and is commonly used to assess the salinity or salinization of soil. Soil conductivity is proportional to the soluble salt content in the soil, so it can be used as a basis for judging soil salt status. * SM: soil moisture % * "Soil moisture" refers specifically to soil volumetric moisture content. The proportion of water in a given volume of soil is usually expressed as a percentage. This index is used to describe the content of water in the soil and is very important for understanding soil water status and plant water supply. * ST: soil temperature °C * "Soil temperature" refers to the temperature inside the soil, which has an important impact on many processes in the soil ecosystem, including microbial activity, decomposition of organic matter, plant growth, and water evaporation. The change in soil temperature can reflect the change in climate conditions. #### Other relevant information: The five inter-seasonal precipitation distribution proportions are +73%, +56%, CK, -56%, and -73%. ## DATA-SPECIFIC INFORMATION FOR: Huang et al.\_ biotic factors 1. Number of variables: 3 2. Number of sheets: 3 3. Number of cases/rows: 2 columns 21 rows/sheet (aboveground biomass (AGB)); 2 columns 21 rows/sheet (belowground biomass (BGB)); 5 columns 21 rows/sheet (coverage) #### Variable List: * AGB: aboveground biomass g/cm² * "Aboveground biomass" refers to the sum of the biomass of all plants living above ground in an ecosystem, usually including tree trunks, branches, leaves, and herbs. This indicator is an important parameter for measuring ecosystem productivity and carbon storage capacity and has important implications for ecology, forestry, and agricultural research. * BGB: belowground biomass g/cm² * "Belowground biomass" refers to the total of plant root biomass. Subsurface biomass is an important component of terrestrial ecosystems and is crucial to understanding the structure and function of ecosystems. * Coverage: % * "Coverage" refers to the projected area of vegetation on the ground as a percentage of the total area. It is a measure of the density of vegetation in an area, reflecting the coverage of vegetation on the ground. #### Other relevant information: The aboveground biomass under -73% treatment is missing two data points due to sample loss, which has been interpolated with the mean and marked in red. Coverage was analyzed and plotted using annual mean values. ## DATA-SPECIFIC INFORMATION FOR: Huang et al.\_ ecosystem CO₂ and H₂O exchange 1. Number of variables: 6 2. Number of sheets: 6 3. Number of cases/rows: 14 columns 21 rows/sheet #### Variable List: * NEE: net ecosystem CO₂ exchange µmol m﹣² s﹣¹ * "Net ecosystem CO₂ exchange" refers to the difference between gross primary productivity (GPP) and ecosystem respiration (ER), reflecting the capacity of ecosystems to absorb or release carbon. * ER: ecosystem respiration µmol m﹣² s﹣¹ * "Ecosystem respiration" refers to the total amount of carbon dioxide released by all living organisms (including plants, animals, and microorganisms) in a given ecosystem through respiration. It is an important part of the ecosystem's carbon cycle and reflects the metabolic activity of organisms in the ecosystem. * GPP: gross primary productivity µmol m﹣² s﹣¹ * "Gross primary productivity" refers to the total amount of energy fixed or organic matter produced by all primary producers (mainly plants) in an ecosystem through photosynthesis over a given period. It is the basis of the energy and material circulation of the ecosystem and is a key indicator to measure the productive capacity of the ecosystem. * ET: evapotranspiration mmol m﹣² s﹣¹ * "Evapotranspiration" refers to the total amount of water lost from the surface to the atmosphere through evaporation and plant transpiration over a given period. * WUE: water use efficiency µmol CO₂ mmol﹣¹ H₂O * "Water use efficiency" refers to the amount of water required by plants to fix each unit mass of carbon dioxide through photosynthesis. It is an indicator of the efficiency of plants in water acquisition and use. * CUE: carbon use efficiency (no units) * "Carbon use efficiency" refers to the use efficiency of each unit of carbon fixed by plants through photosynthesis, usually expressed as the ratio of carbon fixed to carbon absorbed. #### Other relevant information: Because the error of the CUE = -NEE/GPP calculation result is too large, which seriously affects the result, four abnormal CUE values in January and February are excluded, which have been interpolated with the mean and marked in red. ## DATA-SPECIFIC INFORMATION FOR: Huang et al.\_ SEM 1. Number of variables: 11 2. Number of sheets: 1 3. Number of cases/rows: 12 columns 21 rows #### Variable List: As defined above. SPD: seasonal precipitation distribution #### Other relevant information: The SEM model fitting is analyzed by using the simulated precipitation in spring, soil water and salt in spring, and the annual mean value of biotic factors and ecosystem CO₂ and H₂O fluxes. ## DATA-SPECIFIC INFORMATION FOR: Huang et al.\_ Precipitation 1. Number of variables: 0 2. Number of sheets: 1 3. Number of cases/rows: 6 columns 6 rows #### Other relevant information: CK represented the average precipitation (mm) of each quarter from 1988 to 2018; +73% and +56% indicated that the spring precipitation was 73% and 56% higher while summer and autumn precipitation was 73% and 56% lower than the control; -56% and -73% indicated that a 56% and 73% decrease in spring precipitation and a 56% and 73% increase in summer and autumn precipitation compared to the control. Notably, the annual precipitation total and winter precipitation remained constant across the five treatments. ## Sharing/Access information NA ## Code/Software NA
创建时间:
2024-06-28
二维码
社区交流群
二维码
科研交流群
商业服务