欢迎访问《应用生态学报》官方网站,今天是 分享到:

应用生态学报 ›› 2024, Vol. 35 ›› Issue (4): 1007-1015.doi: 10.13287/j.1001-9332.202404.005

• 研究论文 • 上一篇    下一篇

桂北地区不同林龄杉木人工林土壤基质入渗变化及影响因素

杨梦格1, 邓莹莹1, 雷震2, 廖煜亮1, 容清标1, 谭青芳1, 吴沅桓1, 黄钰涵1,3*   

  1. 1广西大学林学院, 广西森林生态与保育重点实验室, 南宁 530004;
    2广西融水县国营贝江河林场, 广西柳州 545000;
    3北京林业大学国家林业与草原局水土保持重点实验室, 北京 100083
  • 收稿日期:2023-12-20 接受日期:2024-02-26 出版日期:2024-04-18 发布日期:2024-10-18
  • 通讯作者: * E-mail: huangyuhan0710@foxmail.com
  • 作者简介:杨梦格, 女, 1999年生, 硕士研究生。主要从事土壤水文研究。E-mail: ymg02122023@163.com
  • 基金资助:
    广西自然科学基金项目(2021GXNSFBA196020)和广西科技基地和人才专项青年创新人才科研专项(桂科AD22035032)

Changes and influence factors of soil matrix infiltration in Chinese fir plantations with different stand ages in northern Guangxi

YANG Mengge1, DENG Yingying1, LEI Zhen2, LIAO Yuliang1, RONG Qingbiao1, TAN Qingfang1, WU Yuanhuan1, HUANG Yuhan1,3*   

  1. 1Guangxi Key Laboratory of Forest Ecology and Conservation, College of Forestry, Guangxi University, Nanning 530004, China;
    2Beijianghe State-owned Forest Farm, Liuzhou 545000, Guangxi, China;
    3Key Laboratory of State Forestry and Grassland Administration on Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China
  • Received:2023-12-20 Accepted:2024-02-26 Online:2024-04-18 Published:2024-10-18

摘要: 土壤基质入渗是人工林获取水分的重要途径,影响着人工林的生态效益和水源涵养能力,目前杉木人工林不同生长阶段土壤基质入渗变化及其影响因素尚不明确。本研究以广西国营贝江河林场杉木人工林(5、8、11和15年)为研究对象,采用表置式环式入渗仪测定土壤基质入渗过程,分析土壤理化性质以明确土壤基质入渗的主导因素。结果表明: 初始入渗率、稳定入渗率和累积入渗量随林龄的增加而增加,不同林龄变化范围分别为141~180 mm·h-1、109~150 mm·h-1和188~251 mm。初始入渗率、稳定入渗率和累积入渗量与土壤毛管孔隙度、有机质、水稳性团聚体、砂粒和黏粒含量呈显著正相关,与土壤容重和粉粒含量呈显著负相关。早期间伐对土壤基质入渗有促进作用,但超过11年后的间伐措施不会进一步促进土壤基质入渗。Philip模型是描述该区域土壤基质入渗过程的最佳模型。综上,在幼龄林到中龄林的生长过程中,杉木人工林的土壤基质入渗能力逐渐提升,在第11年后基质入渗能力趋于稳定;土壤粉粒含量和水稳性团聚体是影响基质入渗的主导因素。

关键词: 入渗, 人工林, 土壤性质, 营林措施

Abstract: Soil matrix infiltration is an important pathway for plantations to obtain water, which affects ecological benefits and water conservation function of plantations. The changes of soil matrix infiltration and its influencing factors in different growth stages of Chinese fir plantations remain unclear. We measured soil matrix infiltration process using a tension infiltrometer in Chinese fir plantations (5, 8, 11, and 15 years old) of Beijiang River Forest Farm in Rongshui, Guangxi, and analyzed soil basic physicochemical properties to identify the dominant factors influencing soil matrix infiltration. The results showed that initial infiltration rate, stable infiltration rate, and cumulative infiltration increased with stand ages. The ranges of different stand ages were 141-180 mm·h-1, 109-150 mm·h-1, and 188-251 mm, respectively. The initial infiltration rate, stable infiltration rate, and cumulative infiltration were significantly positively correlated with soil capillary porosity, soil organic matter, soil water stable macroaggregate, sand content, and clay content, while negatively correlated with soil bulk density and silt content. Early thinning had a positive effect on soil matrix infiltration, but thinning measures after 11 years did not enhance soil matrix infiltration further. Philip model was optimal for describing soil matrix infiltration process in this region. In conclusion, soil matrix infiltration capacity of Chinese fir plantations gradually increased from young to middle-aged stands, but matrix infiltration capacity tended to stabilize after 11 years old. Silt content and water stable macroaggregate were the dominant factors influencing matrix infiltration.

Key words: infiltration, plantation, soil property, forest management measure