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印度干旱亚湿润地区甘蔗(C4)-小麦(C3)生态系统中 CO 通量的动态及其控制环境因素。

Dynamics of CO fluxes and controlling environmental factors in sugarcane (C4)-wheat (C3) ecosystem of dry sub-humid region in India.

机构信息

Indian Institute of Remote Sensing, ISRO, Govt. of India, 4, Kalidas Road, Dehradun, Uttarakhand, 248001, India.

Indian Institute of Space Science and Technology, Thiruvananthapuram, Kerala, 695547, India.

出版信息

Int J Biometeorol. 2021 Jul;65(7):1069-1084. doi: 10.1007/s00484-021-02088-y. Epub 2021 Mar 3.

Abstract

In this study, CO exchange over sugarcane and wheat growing season was quantified by continuous measurement of CO fluxes using eddy covariance (EC) system from January 2014 to June 2015. We also elaborated on the response of CO fluxes to environmental variables. The results show that the ecosystem has seasonal and diurnal dynamics of CO with a distinctive U-shaped curve in both growing seasons with maximal CO absorption reaching up to -8.94 g C m day and -6.08 g C m day over sugarcane and wheat crop, respectively. The ecosystem as a whole acted as a carbon sink during the active growing season while it exhibits a carbon source prior to sowing and post-harvesting of crops. The cumulative net ecosystem exchange (NEE), gross primary productivity (GPP), and ecosystem respiration (R) were -923.04, 3316.65, and 2433.18 g C m over the sugarcane growing season while the values were -192.30, 621.47, and 488.34 g C m over the wheat growing season. The sesbania (green manure) appeared to be a carbon source once it is incorporated into soil. The response of day-time NEE to photosynthetically active radiation (PAR) under two vapor pressure deficit (VPD) sections (0-20 h Pa and 20-40 h Pa) seems more effective over sugarcane (R = 0.41-0.61) as compared to the wheat crop (R = 0.25-0.40). A decrease in net CO uptake was observed under higher VPD conditions. Similarly, night-time NEE was exponentially related to temperature at different soil moisture conditions and showed higher response to optimum soil moisture conditions for sugarcane (R = 0.87, 0.33 ≤ SWC < 0.42 m m) and wheat (R = 0.75, 0.31 ≤ SWC < 0.37 m m) crop seasons. The response of daily averaged NEE to environmental variables through path analysis indicates that PAR was the dominant predictor with the direct path coefficient of -0.65 and -0.74 over sugarcane and wheat growing season, respectively. Satellite-based GPP products from Moderate Resolution Imaging Spectroradiometer (GPP) and Vegetation Photosynthetic model (GPP) were also compared with the GPP obtained from EC (GPP) technique. The seasonal dynamics of GPP and GPP agreed well with each other. This study covers the broad aspects ranging from micro-meteorology to remote sensing over C4-C3 cropping system.

摘要

本研究于 2014 年 1 月至 2015 年 6 月期间,通过涡度相关(EC)系统连续测量 CO 通量,量化了甘蔗和小麦生长季 CO 的交换。我们还阐述了 CO 通量对环境变量的响应。结果表明,生态系统的 CO 具有季节性和日变化,在两个生长季中均呈独特的 U 形曲线,甘蔗和小麦作物的最大 CO 吸收量分别达到-8.94 和-6.08 g C m day。整个生态系统在活跃的生长季表现为碳汇,而在播种前和收获后表现为碳源。甘蔗生长季的净生态系统交换(NEE)、总初级生产力(GPP)和生态系统呼吸(R)分别为-923.04、3316.65 和 2433.18 g C m,而小麦生长季的相应值分别为-192.30、621.47 和 488.34 g C m。Sesbania(绿肥)一旦被纳入土壤,似乎就是一个碳源。在两个水汽压亏缺(VPD)区间(0-20 hPa 和 20-40 hPa)下,日间 NEE 对光合有效辐射(PAR)的响应似乎在甘蔗(R = 0.41-0.61)中比在小麦作物(R = 0.25-0.40)中更有效。在较高 VPD 条件下,净 CO 吸收量下降。同样,夜间 NEE 与不同土壤水分条件下的温度呈指数关系,并表现出对甘蔗(R = 0.87,0.33≤SWC<0.42 m m)和小麦(R = 0.75,0.31≤SWC<0.37 m m)生长季最佳土壤水分条件的更高响应。通过路径分析将日平均 NEE 与环境变量的关系表明,PAR 是主要的预测因子,其直接路径系数分别为-0.65 和-0.74,分别在甘蔗和小麦生长季。还比较了基于卫星的中等分辨率成像光谱仪(GPP)和植被光合作用模型(GPP)的 GPP 产品与 EC(GPP)技术获得的 GPP。GPP 和 GPP 的季节性动态相互吻合。本研究涵盖了从微气象学到 C4-C3 种植系统的遥感等广泛方面。

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