首页> 外文期刊>Current Science: A Fortnightly Journal of Research >Seasonal variability in soil-surface CO2 efflux in selected young tree plantations in semi-arid eco-climate of Madurai.
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Seasonal variability in soil-surface CO2 efflux in selected young tree plantations in semi-arid eco-climate of Madurai.

机译:马杜赖半干旱生态环境中部分幼树人工林土壤表面CO 2 外排的季节变化。

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The response of soil respiration (SR) to varying soil temperature and soil moisture was studied in three-year-old plantation sites of Dalbergia sissoo, Dalbergia latifolia, Albizia lebbeck, Hardwickia binata and Cassiasiamea during 2005-06. Significant seasonal differences in SR rates were observed in each site (P?0.001). The highest rates of soil CO2 efflux were generally found during the rainy season and the lowest during summer in all the study sites. Highest SR rates were found in D. sissoo, 9.89.0.78 .mol m-2 s-1 in November and December, followed by H. binata, 9.68.0.45 .mol m-2 s-1 in September and October 2005, A. lebbeck,8.84.0.43 . m-2 s-1 between November 2005 and January 2006, D. latifolia, 7.6.0.12 . m-2 s-1 in November and December 2005 and C. siamea, 7.3 .mol m-2 s-1 in December 2005.There was a positive and significant (P?0.001) relationship between SR rates and soil moisture in all the sites (r2above 0.60), except C. siamea (r2=0.30). A poor relationship was observed between SR andsoil temperature in all the sites (r2 below 0.2). Examination of the seasonal pattern of SR rates suggests that much of the variability could be attributed to variations in soil moisture. There was a strong indication suggesting that the soil-water deficits served to reduce SR rates during summer and after subsequent rain events. Overall sensitivity of SR rate to soil moisture seems to be good for this semi-arid ecosystem.
机译:在 Dalbergia sissoo , Dalbergia latifolia , Albizia三年的人工林中研究了土壤呼吸(SR)对变化的土壤温度和土壤湿度的响应2005-06年间lebbeck , Hardwickia binata 和 Cassiasiamea 。在每个站点中观察到SR率存在明显的季节性差异( P ?0.001)。在所有研究地点,土壤CO 2 外排率通常最高,而在雨季则最低。在 D中发现最高的SR率。 sissoo ,11月和12月为9.89.0.78 .mol m -2 s -1 ,然后为 H。 binata ,2005年9月和10月, A,9.68.0.45 .mol m -2 s -1 。 lebbeck ,8.84.0.43。 m -2 s -1 在2005年11月到2006年1月之间, D。阔叶植物,7.6.0.22。 m -2 s -1 在2005年11月和12月以及 C。 siamea ,2005年12月为7.3 .mol m -2 s -1 。呈阳性且显着( P ?0.001 ),除了 C,所有位置( r 2 在0.60以上)的SR率与土壤水分之间的关​​系。 siamea ( r 2 = 0.30)。在所有位置,SR与土壤温度之间均存在不良关系( r 2 低于0.2)。对SR率的季节性模式进行的调查表明,大部分变化可能归因于土壤水分的变化。有强烈的迹象表明,土壤水分不足有助于降低夏季和随后的降雨事件后的SR率。对于这个半干旱的生态系统,SR率对土壤水分的总体敏感性似乎很好。

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