Water, Heat and CO2 Transfer over a Salinized Desert in the Arid Area

Expand
  • 1. Fukang Station of Desert Ecology, Xinjiang Institute of Ecology and Geography, CAS, Urumqi 830011, China;
    2. National Institute for Environmental Studies, Tsukuba 305-8506, Japan

Received date: 2003-09-25

  Revised date: 2003-11-22

  Online published: 2004-01-25

Supported by

Integrated Environmental Monitoring Subproject, the Asia-Pacific Environmental Innovation Strategy Project; Knowledge Innovation Project of CAS, No.KZCX3-SW-326

Abstract

An eddy-covariance system and a micrometeorological station were installed at south periphery of Gurbantonggut Desert in April of 2002. Evaluation of the data showed that the measurements of sensible heat (H), latent heat (LE) and CO2 fluxes were reliable. However, a special phenomenon was revealed from detailed analysis on the diurnal and seasonal changes of the fluxes: when LE fluxes signified a strong water shortage and hence severe water stress should have been applied on the plants, CO2 fluxes indicated that the photosynthesis of the plant community was not affected. This was obviously against generally-accepted theory on plant-water relations. No concrete evidence available so far can explain this phenomenon, but we may speculate that local shrub plant might not benefit from the rainfall. Being a salinized desert, its upper soil layer contains high salt content. Thus shrub roots could not develop and survive at upper layer of the soil. On the contrary, roots might develop mainly at deep soil layers near the groundwater table. Therefore, whether rainfall wetted the upper soil layer or not, plant water condition was not affected, but the evapotranspiration (LE) was. The measured change of LE fluxes mainly came from evaporation of soil surface and CO2 fluxes were mainly determined by plant photosynthesis. Since the former is mainly influenced by soil water condition near soil surface and the latter determined by soil water condition near the groundwater table, it is just reasonable that the two aspects are not correlated. Thus, the phenomena reported here occurred under the combined local climatic, botanical and soil conditions and it is not really against the principle of plant-water relations in general.

Cite this article

LI Yan, WANG Qinxue, MA Jian, WATANABE Masataka, ZHANG Xiaolei . Water, Heat and CO2 Transfer over a Salinized Desert in the Arid Area[J]. Acta Geographica Sinica, 2004 , 59(1) : 33 -39 . DOI: 10.11821/xb200401004

References


[1] Baldocchi D, Meyers T. On using eco-physiological, micrometeorological and biogeochemical theory to evaluate carbon dioxide, water vapor and trace gas fluxes over vegetation. Agricultural and Forest Meteorology, 1998, 90: 1-25.

[2] Ke Xiaoxin, Yang Xingguo, Zhang Xudong. Micrometeorological methods for measuring and estimating evapotranspiration over farmland. Arid Land Agricultural Research, 1995, 13:31-40.
[柯晓新, 杨兴国, 张旭东. 农田蒸散测算的微气象学方法. 干旱地区农业研究, 1995, 13: 31-40.]

[3] Zhang Yongqian, Shen Yanjun, Liu Changming et al. Measurement and analysis of water, heat and CO2 flux from a farmland in the North China Plain. Acta Geographica Sinica, 2002, 57(3): 332-342.
[张永强, 沈彦俊, 刘昌明 等. 华北平原典型农田水、热与CO2通量的测定. 地理学报, 2002, 57(3): 332-342.]

[4] Law B E, Falge E, Gu L et al. Environmental controls over carbon dioxide and water vapor exchange of terrestrial vegetation. Agricultural and Forest Meteorology, 2002, 113: 92-120.

[5] Meyers T P. A comparison of summertime water and CO2 fluxes over rangeland for well watered and drought conditions. Agricultural and Forest Meteorology, 2001, 106: 205-214.

[6] Hunt J E, Kelliher F M, McSeveny T M et al. Evaporation and carbon dioxide exchange between the atmosphere and a tussock grassland during a summer drought. Agricultural and Forest Meteorology, 2002, 111: 65-82.

[7] Twine T E, Kustas W P, Norman J M et al. Correcting eddy-covariance flux underestimating over a grassland. Agricultural and Forest Meteorology, 2000, 103: 279-300.

[8] Emmerich W E. Carbon dioxide fluxes in a semiarid environment with high carbonate soils. Agricultural and Forest Meteorology, 2003, 116: 91-102.

[9] Lal R. Potential of desertification control to sequester carbon and mitigate the greenhouse effect: review. Climatic Change, 2001, 51: 35-72.

[10] Feng Q, Cheng GD, Masao M. The carbon cycle of sandy lands in China and its significance. Climatic Change, 2001, 48: 535-549.

Outlines

/