Xie Ting-Ting, Su Pei-Xi, Gao Song
Plant Stress Ecophysiology and Biotechnology Laboratory, Linze Inland River Basin Research Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China.
Ying Yong Sheng Tai Xue Bao. 2010 Jun;21(6):1425-31.
The measurement system of Li-8100 carbon flux and the modified assimilation chamber were used to study the photosynthetic characteristics of cotton (Gossypium hirsutum L.) canopy in the oasis edge region in middle reach of Heihe River Basin, mid Hexi Corridor of Gansu. At the experimental site, soil respiration and evaporation rates were significantly higher in late June than in early August, and the diurnal variation of canopy photosynthetic rate showed single-peak type. The photosynthetic rate was significantly higher (P < 0.01) in late June than in early August, with the daily average value being (43.11 +/- 1.26) micromol CO2 x m(-2) x s(-1) and (24.53 +/- 0.60) micromol CO2 x m(-2) x s(-1), respectively. The diurnal variation of canopy transpiration rate also presented single-peak type, with the daily average value in late June and early August being (3.10 +/- 0.34) mmol H2O x m(-2) x s(-1) and (1.60 +/- 0.26) mmol H2O x m(-2) x s(-1), respectively, and differed significantly (P < 0.01). The daily average value of canopy water use efficiency in late June and early August was (15.67 +/- 1.77) mmol CO2 x mol(-1) H2O and (23.08 +/- 5.54) mmol CO2 x mol(-1) H2O, respectively, but the difference was not significant (P > 0.05). Both in late June and in early August, the canopy photosynthetic rate was positively correlated with air temperature, PAR, and soil moisture content, suggesting that there was no midday depression of photosynthesis in the two periods. In August, the canopy photosynthetic rate and transpiration rate decreased significantly, because of the lower soil moisture content and leaf senescence, but the canopy water use efficiency had no significant decrease.
利用Li-8100碳通量测量系统和改良同化箱,对甘肃河西走廊中部黑河中游绿洲边缘地区棉花(陆地棉)冠层光合特性进行了研究。在试验地,6月下旬土壤呼吸速率和蒸发速率显著高于8月上旬,冠层光合速率日变化呈单峰型。6月下旬光合速率显著高于8月上旬(P<0.01),日均值分别为(43.11±1.26)μmol CO2·m-2·s-1和(24.53±0.60)μmol CO2·m-2·s-1。冠层蒸腾速率日变化也呈单峰型,6月下旬和8月上旬日均值分别为(3.10±0.34)mmol H2O·m-2·s-1和(1.60±0.26)mmol H2O·m-2·s-1,差异显著(P<0.01)。6月下旬和8月上旬冠层水分利用效率日均值分别为(15.67±1.77)mmol CO2·mol-1H2O和(23.08±5.54)mmol CO2·mol-1H2O,但差异不显著(P>0.05)。6月下旬和8月上旬,冠层光合速率均与气温、光合有效辐射和土壤含水量呈正相关,表明这两个时期不存在光合午休现象。8月,由于土壤含水量降低和叶片衰老,冠层光合速率和蒸腾速率显著下降,但冠层水分利用效率无显著降低。