Elevated Temperature and Carbon Dioxide alter the Tea Rhizosphere Soil Dynamics

A. S. Rahman, Jayanta Barukial, Satya Ranjan Sarmah, R. D. Baruah
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Abstract

Aim: Aim: The aim of this work is to explore the impact of climate change on the tea rhizosphere soil dynamics. The experiment sought to study the tea rhizosphere Soil Organic Carbon (SOC), Total Nitrogen (TN), Microbial Biomass Carbon (MBC) and Microbial Biomass Nitrogen (MBN) under elevated levels of temperature and Carbon Dioxide (CO 2 ). Materials and Methods: Materials and Methods: The experimental design was set up with two Open Top Chamber (OTC) facilities, creating localized conditions with increased temperature and CO 2. Both temperature and CO 2 were elevated in OTC-1 (eTemp+eCO 2 ), with CO 2 concentration of 550 ppm, while in OTC-2 (eTemp), only the temperature was elevated. Temperature was 1.5-2ºC higher than ambient. Four tea cultivars (TV1, TV20, TV22 and TV23) were placed inside the OTCs and rhizosphere soil samples were collected at regular intervals. Results: Results: The results indicated that in eTemp+eCO 2 treatment, over the period of time, the rate of change in SOC showed significant increase ( p< 0.01 ) compared to control, while TN showed no significant variations, the rate of change in MBC showed significant increase ( p< 0.05 ) in eTemp treatment. No significant variation was observed in the rate of change in MBN. Overall, SOC and MBC, after 300 hr of treatments showed significant increase ( p <0.001) in both eTemp and eTemp+eCO 2 treatments when compared to control. However, after 300 hr of treatment overall soil TN exhibited a significant increase ( p <0.05) in eTemp+eCO 2 treatment. Conclusion: Conclusion: This study addresses the research gap through an evidence based experimental work that monitors the impact of temperature and CO 2 on tea rhizosphere. From the study, it can be concluded that elevated temperature and CO 2 alter the rate of change in soil organic carbon pool of tea rhizosphere soil along with the accumulation of biomass carbon, whereas no such alteration was found for microbial biomass nitrogen.
温度升高和二氧化碳改变了茶叶根瘤菌土壤动力学
目的:本工作旨在探索气候变化对茶叶根圈土壤动力学的影响。实验旨在研究在温度和二氧化碳(CO 2)水平升高的条件下,茶叶根瘤菌圈土壤有机碳(SOC)、全氮(TN)、微生物生物量碳(MBC)和微生物生物量氮(MBN)的变化情况。材料与方法材料与方法:实验设计采用了两个开放式箱体(OTC)设施,创造了温度和二氧化碳升高的局部条件。在 OTC-1(eTemp+eCO 2)中,温度和 CO 2 均升高,CO 2 浓度为 550 ppm,而在 OTC-2(eTemp)中,只升高温度。温度比环境温度高 1.5-2ºC 。四个茶树品种(TV1、TV20、TV22 和 TV23)被置于 OTC 中,并定期采集根圈土壤样本。结果结果结果表明,在 eTemp+eCO 2 处理中,随着时间的推移,与对照相比,SOC 的变化率显著增加(p< 0.01),而 TN 的变化不显著;在 eTemp 处理中,MBC 的变化率显著增加(p< 0.05)。MBN 的变化率没有观察到明显变化。总体而言,与对照组相比,处理 300 小时后,eTemp 和 eTemp+eCO 2 处理中的 SOC 和 MBC 都有明显增加(p <0.001)。然而,经过 300 小时的处理后,eTemp+eCO 2 处理的土壤总氨显著增加(p <0.05)。结论结论本研究通过循证实验工作,监测温度和二氧化碳对茶叶根瘤菌的影响,填补了研究空白。从研究中可以得出结论,温度升高和二氧化碳会改变茶叶根瘤土壤有机碳库的变化速率以及生物量碳的积累,而微生物生物量氮则没有这种变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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