干热河谷失稳性坡面植物碳氮磷化学计量特征对土壤性质的响应

以干热河谷阴坡和阳坡典型失稳性坡面不同区段(稳定区、失稳区和堆积区)的草本植物为研究对象,分析植物地上和地下碳(C)、氮(N)、磷(P)含量及其化学计量特征对土壤性质的响应机制。结果表明:失稳性坡面植物地上C含量(320.59 g·kg^-1)、N含量(12.15 g·kg^-1)和C/P(25.37)均显著高于地下(分别为254.01 g·kg^-1、6.12 g·kg^-1、13.43),C/N则表现为地下(43.09)显著高于地上(31.90)。阳坡植物地上和地下C含量、N/P均表现为稳定区和失稳区显著高于堆积区,N含量则表现为失稳区显著高于堆积区;阴坡植物地上N、P含量及地下P含量均表现为堆积区显著高于稳定区和失稳区,地下C含量则反之。植物地上生长主要受P限制,根系生长主要受N限制并随区段向下呈逐渐增加趋势;阴坡植物生长受P的限制程度高于阳坡,N限制弱于阳坡。土壤含水量(SWC)是影响植物地上C、N、P含量变化的重要因子,影响值分别为28.8%、20.8%、19.9%,土壤有机碳(SOC)则显著影响植物地下C、N含量,影响值分别为49.5%、22.1%,植物地下N含量的变化主要受土壤pH值的影响(24.3%)。坡向、区段及土壤因子均显著影响植物养分的分配,SWC和SOC是主要影响因子,同时还受土壤pH值的影响。

Responses of plant C:N:P stoichiometry to soil properties on unstable slopes of dry-hot valley

In this study, we examined plant C:N:P stoichiometry of herbaceous plants in different sections (stable area, unstable area and deposition area) of the unstable slope on both shade and sunny aspects of dry-hot valley with different soil properties. The results showed that C concentration (320.59 g·kg^-1), N concentration (12.15 g·kg^-1), and N:P ratio (25.37) of shoot on the unstable slope were significantly higher than those of root, with 254.01 g·kg^-1, 6.12 g·kg^-1 and 13.43, respectively. The average value of the C:N ratio was significantly higher in root (43.09) than shoot (31.90). The C content and N:P ratio of shoot and root in stable and unstable areas were significantly higher than in deposition area, whereas the N content in unstable area was significantly higher than that in deposition area on the sunny slope. In addition, the N and P contents of shoot and the root P content in deposition area were significantly higher than in stable and unstable areas, whereas the C content of root in stable and unstable areas were significantly higher than in deposition area on the shade slope. Moreover, the shoot growth of plants was mainly limited by P, whereas root growth was mainly limited by N and the limitation gradually increased as the section goes down. Soil water content (SWC) was an important factor controlling the C, N, and P contents change of shoot with the relative influence ratios of 28.8%, 20.8%, and 19.9%, respectively. Soil organic carbon (SOC) had a significant impact on the C and P contents of root with the relative influence ratios of 49.5% and 22.1%. The change of root N content was mainly affected by soil pH (24.3%). Our results revealed that nutrient allocation of plant was significantly affected by slope aspects, sections and soil factors, which were mainly constituted by SWC, SOC, and soil pH.