哈尼梯田湿地土壤不同形态磷的时空分布特征
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

云南省基础研究重点项目(202001AS070042);国家自然科学基金项目(41371066);云南省高原湿地保护修复与生态服务重点实验室开放基金项目(202105AG070002)


Spatiotemporal distribution characteristics of different forms of phosphorus in soils of Hani terrace wetland
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 文章评论
    摘要:

    磷是湿地和农业生态系统中的重要元素之一,其中土壤磷形态的迁移转化广受关注。以哈尼梯田湿地为例,分别在哈尼梯田湿地的水稻生长期、收获期和休闲期,采集湿地不同海拔(梯田区上部、中部和下部)和不同深度的土壤(0-20 cm,20-40 cm,40-60 cm,60-80 cm)进行磷形态分析,研究了哈尼梯田湿地土壤中不同形态磷的时空分布规律和影响因素。结果表明:(1)哈尼梯田湿地土壤中总磷(TP)含量均值为318.74 mg/kg,在水稻收获期含量最高,无机磷(IP)含量均值在水稻休闲期最高(85.95 mg/kg),湿地土壤磷总体呈缺乏状态。(2)受外源磷输入影响,铁铝结合态磷(NaOH-P)占无机磷比重最大,且季节差异性显著(P<0.05);而钙结合态磷(HCl-P)在各季节无显著差异(P>0.05),这与湿地生态环境和地质背景有关。(3)哈尼梯田湿地对磷的迁移有截留作用,表现为各形态磷含量总体呈现在上部梯田湿地较高,并随海拔的降低而降低;不同形态磷含量在20-40 cm土层富集。(4)除HCl-P外,其余形态磷与土壤粒径在不同土层表现为负相关;不同土层TP和有机磷(OP)与pH值呈正相关;土壤总有机碳(TOC)与不同形态磷在收获期呈显著负相关(P<0.05)。研究表明了哈尼梯田湿地立体空间结构和人为活动能影响湿地生态系统中磷的分布与迁移循环,该结论可为梯田湿地的可持续发展提供参考。

    Abstract:

    Phosphorus is an important element of the wetland and agricultural ecosystems, and great attention has been paid to the movement and transformation of phosphorus speciation in soils. The Hani terrace, which is located in Yunnan, a province in southwest China, is unique with its typical mountainous landscape of forests, villages, man-made paddy wetlands and rivers. The aim of the research was to investigate the spatiotemporal distribution of various forms of phosphorus in the soils of Hani terrace wetland and find out its influencing factors. In view of that, this paper conducted a comprehensive analysis of the forms of phosphorus in the soils collected at different altitudes (the upper, middle, and lower terrace areas) and depths (0-20 cm, 20-40 cm, 40-60 cm, 60-80 cm) in the growing, harvest and fallow periods of paddy, respectively. The results indicated that (1) in the soils of Hani terrace wetland, the average content value of total phosphorus (TP) was 318.74 mg/kg and reached its peak in the harvest period. The average content value of inorganic phosphorus (IP) was the highest in the fallow period (85.95 mg/kg), generally presenting a deficiency of phosphorus in the wetland soils. (2) due to the impact of exogenous phosphorus input, iron/aluminum-bound phosphorus (NaOH-P) made up the largest part of IP and showed significant seasonal differences as regards its content (P<0.05). Whereas, the content of calcium-bound phosphorus (HCI-P) had no significant difference in each season (P>0.05), which was related to the ecological environment and geological background of the wetland. (3) Hani terrace wetland could intercept the movement of phosphorus, manifested in that the contents of various forms of phosphorus were generally higher in the upper terrace area and decreased with the decrease of altitude. In vertical soil profiles, the enrichment of phosphorus in different forms occurred in the 20-40 cm soil layer. (4) all the forms of phosphorus, except HCI-P, were negatively correlated with soil particle size in different soil layers. The TP and organic phosphorus (OP) were positively correlated with pH in different soil layers. There was significant negative correlation between soil total organic carbon (TOC) and different forms of phosphorus during the harvest period (P<0.05). Based on the findings summarized above, the research showed that the stereoscopic spatial structure of Hani terrace wetland and human activities could influence phosphorus distribution and cycling in the wetland ecosystem, which could provide a reference for the sustainable development of terrace wetlands.

    参考文献
    相似文献
    引证文献
引用本文

夏欣,宋维峰,彭正耀.哈尼梯田湿地土壤不同形态磷的时空分布特征.生态学报,2024,44(2):676~685

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数: