Yan Bang Guo, He Guang Xiong, Shi Liang Tao, Fan Bo, Li Ji Chao, Pan Zhi Xian, Ji Zhong Hua
Institute of Tropical Eco-agricul-tural Sciences, Yunnan Academy of Agricultural Sciences, Yuanmou 651300, Yunnan, China.
Institute of Agricultural Environment and Resources, Yunnan Academy of Agricultural Sciences, Kunming 650205, China.
Ying Yong Sheng Tai Xue Bao. 2016 Apr 22;27(4):1039-1045. doi: 10.13287/j.1001-9332.201604.002.
By performing a pot experiment, the study compared leaf and litter element concentration between the dry-red soil and vertisols, and analyzed the interactive effects of soil types and species on leaf nutrient concentration and nutrient resorption efficiency. The results showed that the soil type significantly affected the concentrations of N, P, Ca, Mg, Cu, Zn, Fe and N:P in leaves as well as the concentrations of N, P, Mn and N:P in leaf litters. Concentrations of N, Mn and N:P in leaves and litters derived from the dry-red soil were significantly higher than those from the vertisols. In contrast, concentrations of P, Ca, Mg, Fe, Cu and Zn in leaves and concentration of P in litters derived from the dry-red soil were significantly lower than those from the vertisols. Leaf N concentration was 34.8% higher, and leaf P concentration was 40.0% lower from the dry-red soil compared with those from the vertisols. N, P and K showed net resorption while the other elements showed accumulating patterns when leaf was senesced. Accumulation of Ca, Mg and Mn of senesced leaves was significantly higher on the dry-red soil than on the vertisols. Species identities only significantly affected leaf N concentration. Interactions of species and soil taxonomy significantly affected nutrient concentration neither in leaves nor in leaf litters, indicating that soil taxonomy influenced plant nutrient concentration in a similar way across multiple species. The influences of soil types on plant element concentration could have further effects on litter decomposition, plant-soil nutrient feedback and biogeochemical cycle in this dry and hot valley.
通过进行盆栽试验,该研究比较了燥红土和变性土之间叶片及凋落物的元素浓度,并分析了土壤类型和物种对叶片养分浓度及养分再吸收效率的交互作用。结果表明,土壤类型显著影响叶片中氮、磷、钙、镁、铜、锌、铁的浓度以及氮磷比,还有凋落物中氮、磷、锰的浓度以及氮磷比。来自燥红土的叶片和凋落物中氮、锰的浓度以及氮磷比显著高于来自变性土的。相反,来自燥红土的叶片中磷、钙、镁、铁、铜和锌的浓度以及凋落物中磷的浓度显著低于来自变性土的。与来自变性土的相比,来自燥红土的叶片氮浓度高34.8%,磷浓度低40.0%。叶片衰老时,氮、磷和钾表现出净再吸收,而其他元素则表现出积累模式。衰老叶片中钙、镁和锰在燥红土上的积累显著高于在变性土上的。物种特性仅显著影响叶片氮浓度。物种与土壤分类的相互作用对叶片和凋落物中的养分浓度均无显著影响,这表明土壤分类对多种物种的植物养分浓度影响方式相似。土壤类型对植物元素浓度的影响可能会对这个干热河谷中的凋落物分解、植物 - 土壤养分反馈和生物地球化学循环产生进一步影响。