Temporal and Spatial Variations in Carbon Flux and Their Influencing Mechanisms on the Middle Tien Shan Region Grassland Ecosystem, China

Author:

Zhang Kun1234,Wang Yu2356,Mamtimin Ali2356ORCID,Liu Yongqiang14,Gao Jiacheng2356,Aihaiti Ailiyaer2356,Wen Cong2356,Song Meiqi2356,Yang Fan2356,Zhou Chenglong2356,Huo Wen2356ORCID

Affiliation:

1. College of Geography and Remote Sensing Sciences, Xinjiang University, Urumqi 830046, China

2. Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China

3. National Observation and Research Station of Desert Meteorology, Taklimakan Desert of Xinjiang, Urumqi 830002, China

4. Xinjiang Key Laboratory of Oasis Ecology, Xinjiang University, Urumqi 830046, China

5. Taklimakan Desert Meteorology Field Experiment Station, China Meteorological Administration, Urumqi 830002, China

6. Xinjiang Key Laboratory of Desert Meteorology and Sandstorm, Urumqi 830002, China

Abstract

Grassland ecosystems are an important component of global terrestrial ecosystems and play a crucial role in the global carbon cycle. Therefore, it is important to study the carbon dioxide (CO2) process in the Middle Tien Shan grassland ecosystem, which can be regarded as a typical representative of the mountain grasslands in Xinjiang. Eddy covariance (EC) and the global carbon fluxes dataset (GCFD) were utilized to continuously monitor the Middle Tien Shan grassland ecosystem in Xinjiang throughout the 2018 growing season. The findings revealed notable daily and monthly fluctuations in net ecosystem exchange (NEE), gross primary productivity (GPP), and ecosystem respiration (Reco). On a daily basis, there was net absorption of CO2 during the day and net emission during the night. The grassland acted as a carbon sink from 6:00 to 18:00 and as a carbon source for the remaining hours of the day. On a monthly scale, June and July served as carbon sinks, whereas the other months acted as carbon sources. The accumulated NEE, GPP, and Reco during the growing season were −329.49 g C m−2, 779.04 g C m−2, and 449.55 g C m−2, respectively. On the half-hourly and daily scales, soil temperature (Ts) was the main contributor to CO2 fluxes and had the greatest influence on the variations in CO2 fluxes. Additionally, air temperature (Ta) showed a strong correlation with CO2 fluxes. The grassland ecosystems exhibited the strongest CO2 uptake, reaching its peak at soil temperatures of 25 °C. Moreover, as the air temperatures rose above 15 °C, there was a gradual decrease in NEE, while CO2 uptake increased. The applicability of GCFD data is good in the grassland ecosystem of the Middle Tien Shan Mountains, with correlations of 0.59, 0.81, and 0.73 for NEE, GPP, and Reco, respectively, compared to field observations. In terms of remote sensing spatial distribution, the Middle Tien Shan grassland ecosystem exhibits a carbon sink phenomenon.

Funder

The Special Project for the Construction of Innovation Environment in the Autonomous Region

The Special Funds for Basic Scientific Research Business Expenses of Central-level Public Welfare Scientific Research Institutes

The Scientific and Technological Innovation Team (Tien Shan Innovation Team) project

The National Natural Science Foundation of China

The S&T Development Fund of IDM

The Graduate Education Innovation Program of the Autonomous Region

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

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