Liao JianXiong, Hou ZongDong, Wang GenXuan
State Key Laboratory of Arid Agroecology, Lanzhou University, and Shapotou Desert Research and Experiment Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, 730 000, People's Republic of China.
State Key Laboratory of Arid Agroecology, Lanzhou University, and Shapotou Desert Research and Experiment Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, 730 000, People's Republic of China.Corresponding author; email:
Funct Plant Biol. 2002 Jul;29(7):891-897. doi: 10.1071/PP01168.
The effects of elevated CO2 concentration and drought on the chemical composition and decomposition of spring wheat (Triticum aestivum L.) leaf litter were investigated. The results obtained were as follows: (i)decomposition of leaf litter material grown under elevated CO2 and drought (ED) was significantly reduced (P=0.007), but no significant changes occurred under elevated CO2 (EW) (P=0.203) or drought (AD) (P=0.599). The loss of mass of leaf litter material decomposing under ambient CO2 (AW) was higher than that under AD and ED, but the difference between AW and EW was insignificant (P=0.318); (ii) compared with leaf litter material from plants grown under AW, ED litter had higher total C content, despite decreased soluble carbohydrates, and lower total N content, and hence increased C/N ratio; (iii) tannins and lignin were not significantly correlated with the loss of mass, but increased concentrations of lignin and tannins in the decomposing wheat material might reduce the rate of litter turnover in later stages of decomposition; (iv) the decreased decomposition rate at ED was the result of an increase in the C/N ratio, a decrease in total N content, and inhibition of soil microbial activity by drought. So there will be the need to increase external N inputs and decrease stalks to the spring wheat field to increase decomposition rates if CO2 concentration increases and semi-arid regions become drier in the future.
研究了二氧化碳浓度升高和干旱对春小麦(Triticum aestivum L.)凋落物化学成分及分解的影响。得到的结果如下:(i)在二氧化碳浓度升高和干旱(ED)条件下生长的凋落物材料分解显著降低(P = 0.007),但在二氧化碳浓度升高(EW)(P = 0.203)或干旱(AD)(P = 0.599)条件下未发生显著变化。在环境二氧化碳(AW)条件下分解的凋落物材料质量损失高于AD和ED条件下的,但AW和EW之间的差异不显著(P = 0.318);(ii)与在AW条件下生长的植物的凋落物材料相比,ED凋落物总碳含量较高,尽管可溶性碳水化合物减少,总氮含量较低,因此碳氮比增加;(iii)单宁和木质素与质量损失无显著相关性,但分解的小麦材料中木质素和单宁浓度增加可能会降低后期分解阶段的凋落物周转速率;(iv)ED条件下分解速率降低是碳氮比增加、总氮含量降低以及干旱对土壤微生物活性抑制的结果。因此,如果未来二氧化碳浓度增加且半干旱地区变得更加干燥,将需要增加春小麦田的外部氮输入并减少秸秆量以提高分解速率。