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Soil CO2 flux and its environmental affecting factors in a saline desert.

MA Jie1,2,3, YU Dan-dan3,4, ZHENG Xin-jun1,2**   

  1. (1State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Science, Urumqi 830011, China; 2Fukang Station of Desert Ecology, Chinese Academy of Sciences, Fukang 831505, Xinjiang, China; 3University of Chinese Academy of Sciences, Beijing 100049, China; 4Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China)
  • Online:2013-10-10 Published:2013-10-10

Abstract: Taking the southern Gurbantunggut Desert in Xinjiang as the object, and by using LI-8150 multichannel soil CO2 flux system, a continuous measurement of surface soil CO2 flux under Tamarix ramosissima population in an original saline desert was conducted during growth season, with the diurnal and seasonal variations of the CO2 flux and related environmental affecting factors analyzed. During the whole growth season of the population, the diurnal variation of the CO2 flux presented two distinct patterns, one was single-peaked, and the other was bimodal. The difference in the diurnal variation of the CO2 flux could be mainly caused by the inhibition of soil microbial activity by high temperature. The seasonal variation of the CO2 flux was not apparent, being fluctuated within a stable range (0.13-0.3 g C·m-2·d-1) especially when the diurnal variation was bimodal. When rainfall events happened, the CO2 flux increased in impulse type. During the rainfall cycle, the diurnal CO2 flux varied in bimodal-singlepeaked-bimodal type. Soil moisture content was the main factor limiting the soil CO2 flux in the saline desert.

Key words: DNA damage., tissue damage, Pagrosomus major, deltamethrin, comet assay