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Environmental controls and influences of Pinus roxburghii Sarg. (Chir pine) plantation on temporal variation in soil carbon dioxide emission and soil organic carbon stock under humid subtropical region
Environmental Monitoring and Assessment ( IF 2.9 ) Pub Date : 2021-09-06 , DOI: 10.1007/s10661-021-09419-x
S Sivaranjani 1 , Vijender Pal Panwar 1
Affiliation  

Soil carbon dioxide emission is a major component of ecosystem respiration, responsible for organic carbon losses from the ecosystem. In Pinus roxburghii Sarg. plantations, higher CO2 emission coincided with maximum soil moisture and soil temperature during the rainy season (4.23 µmol CO2m-2 s-1) followed by summer season (1.69 µmol CO2m-2 s-1) and winter season (1.35 µmol CO2m-2 s-1). The soil CO2 emission rates recorded during the rainy season differed significantly from other seasons (p < 0.05). Multiple linear regression revealed that rainfall was the main dominant factor affecting the soil CO2 emission. A significant positive correlation with minimum air temperature and average air temperature during the lag period, i.e., preceding 15 days of data, was recorded. A significant positive correlation was also observed between annual soil CO2 emission rates with soil temperature, soil moisture, air temperature, and rainfall (p < 0.05). Vapor pressure and relative humidity at 14.19 h also emerged as additional scientific variables affecting soil CO2 emission with significant positive correlations. Annual soil CO2 emission rates and soil properties were not significantly correlated but were positively correlated with organic carbon, exchangeable potassium and negatively correlated with available nitrogen and phosphorous (p > 0.05). Higher annual average carbon stock, 95.05 t ha-1 in P. roxburghii plantations than the yearly soil CO2 emission, 33.23 t ha-1 indicates that plantations sequester more carbon than the emissions.



中文翻译:

Pinus roxburghii Sarg 的环境控制和影响。亚热带湿润地区(赤松)人工林土壤二氧化碳排放和土壤有机碳储量的时间变化

土壤二氧化碳排放是生态系统呼吸的主要组成部分,是生态系统有机碳流失的主要原因。在Pinus roxburghii Sarg 中。在人工林中,较高的 CO 2排放与雨季(4.23 µmol CO 2 m -2  s -1)其次是夏季(1.69 µmol CO 2 m -2  s -1)和冬季( 1.35 µmol CO 2 m -2  s -1 )。雨季记录的土壤CO 2排放率与其他季节显着不同(p < 0.05)。多元线性回归表明降雨是影响土壤CO 2排放的主要主导因素。记录了滞后期(即数据的前 15 天)与最低气温和平均气温的显着正相关。土壤CO 2 年排放率与土壤温度、土壤湿度、气温和降雨量之间也存在显着的正相关(p  < 0.05)。14.19 小时的蒸气压和相对湿度也作为影响土壤 CO 2排放的附加科学变量出现,具有显着的正相关性。年土壤 CO 2排放率与土壤性质无显着相关,但与有机碳、交换性钾呈正相关,与有效氮、磷呈负相关(p  > 0.05)。更高的年平均碳股票,95.05吨公顷-1P.莲种植园比每年土壤CO 2排放,33.23吨公顷-1表示种植园封存比排放更多的碳。

更新日期:2021-09-07
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