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应用生态学报 ›› 2021, Vol. 32 ›› Issue (11): 4004-4010.doi: 10.13287/j.1001-9332.202111.028

• 研究论文 • 上一篇    下一篇

蒙东地区水肥耦合对紫花苜蓿土壤磷组分的影响

张艾明1,2*,徐玉梅1,朱建宇1,余洪茜1,刘苏蓝1   

  1. 1赤峰学院资源环境与建筑工程学院, 内蒙古赤峰 024000;
    2赤峰学院农业科学研究院, 内蒙古赤峰 024000
  • 出版日期:2021-11-15 发布日期:2022-05-15
  • 通讯作者: *E-mail: zhangaiming888@126.com
  • 作者简介:张艾明, 女, 1983年生, 博士, 讲师。主要从事土壤环境与植物营养研究。E-mail:zhangaiming888@126.com
  • 基金资助:
    本文由赤峰学院科技特派项目(cfxyfd201620)、赤峰学院农业科学研究院项目(cfxynky201902)、赤峰学院环境演变与灾害应急管理研究科研创新团队项目(cfxykycxtd202006)和赤峰学院土壤环境与植物营养科研实验室项目资助

Effects of the coupling water and fertilizer on soil phosphorus components in alfalfa field in Eastern Inner Mongolia, China

ZHANG Ai-ming1,2*, XU Yu-mei1, ZHU Jian-yu1, YU Hong-xi1, LIU Su-lan1   

  1. 1School of Resources, Environment and Architectural Engineering, Chifeng University, Chifeng 024000, Inner Mongolia, China;
    2Academy of Agricultural Sciences, Chifeng University, Chifeng 024000, Inner Mongolia, China
  • Online:2021-11-15 Published:2022-05-15
  • Supported by:
    This work was supported by the Science and Technology Special Project of Chifeng University (cfxyfd201620), the Academy of Agricultural Sciences Project of Chifeng University (cfxynky201902), the Project of Innovative Teams of Environmental Evolution and Disaster Emergency Management Research of Chifeng University (cfxykycxtd202006), and the Project of Soil Environment and Plant Nutrition Research Laboratory of Chifeng University.

摘要: 磷素在土壤中可分为有机磷和无机磷两大组分,不同形态的磷供给植物营养的难易程度不同,应用液体31P核磁共振技术(31P-NMR)探明土壤磷组分可为进一步调控土壤磷营养提供重要的理论依据。本研究采用盆栽试验,以紫花苜蓿和栗钙土为对象,设置常规和干旱水分处理,并设置不同的施磷水平(P0~P4:0、0.025、0.05、0.1、0.2 g P2O5·kg-1土),应用液体31P-NMR技术测定土壤磷组分,研究水肥耦合条件下紫花苜蓿土壤磷组分特征。结果表明: 不同水肥条件下,土壤无机磷主要包括无机正磷酸盐、无机焦磷酸盐和无机多磷酸盐。无机正磷酸盐在土壤无机磷组分中占主导地位,干旱会降低无机正磷酸盐含量;无机焦磷酸盐和无机多磷酸盐可存在于高施磷水平(P4)的土壤中。有机磷组分中,正磷酸单酯占主导地位,干旱影响紫花苜蓿对土壤中正磷酸单酯的转化和利用。综上,合理的水肥管理可对蒙东地区紫花苜蓿土壤磷营养的转化和利用进行有效的调控。

关键词: 水肥耦合, 31P-NMR, 紫花苜蓿, 磷组分

Abstract: Soil phosphorus (P) could be categorized into organic and inorganic forms, with diffe-rent capabilities of nutrient supply. Exploring soil P components through liquid 31P-NMR would provide an important theoretical basis for soil P nutrition regulation. This study addressed the characteristic of P in alfalfa (Medicago sativa) soil via the pot experiment. There were two scenarios of treatments with conventional and dry water combined with different P fertilizer levels (P0-P4: 0, 0.025, 0.05, 0.1, and 0.2 g P2O5·kg-1soil). The characteristics of P components in alfalfa soil under water-fertilizer coupling conditions were measured by liquid 31P-NMR. Results showed that under different water and fertilizer treatments, soil inorganic P was mainly composed of inorganic orthophosphate, pyrophosphate and inorganic polyphosphate. Inorganic orthophosphate was the dominant component of inorganic P, which could be reduced by drought. High P application (P4) could increase the contents of soil inorganic polyphosphates and inorganic pyrophosphates. Among the organic P components, monoester orthophosphate was dominant, the conversion and utilization of which in alfalfa soil were affected by drought. Overall, the rational management of water and fertilizer could effectively regulate the conversion and utilization of P nutrients in alfalfa soil in Eastern Inner Mongolia.

Key words: water-fertilizer coupling, 31P-NMR, alfalfa, phosphorus component.