浙江安吉三种典型林分类型下土壤入渗特征及其影响因素
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S152.7

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国家自然科学基金项目(32271964)资助。


Soil Infiltration Characteristics and Influential Factors Under Three Typical Forest Stand Types in Anji County of Zhejiang Province
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    摘要:

    本研究利用表置式双环测定仪测定了浙江安吉3种典型林分类型(毛竹纯林、毛竹–杉木混交林、杉木纯林)的入渗性能,并分析了土壤性质和根系特征对土壤入渗速率的影响。结果表明:①初始入渗速率(947.7 ~ 1 220.5 mm/h)、第1阶段入渗速率(612.6 ~ 751.6 mm/h)、第2阶段入渗速率(479.0 ~ 591.3 mm/h)、第3阶段入渗速率(352.9 ~ 433.4 mm/h)、稳定入渗速率(272.0 ~ 369.0 mm/h)、平均入渗速率(373.1 ~ 498.2 mm/h)均随着毛竹入侵程度的增加而增加,除初始入渗速率外,其他入渗速率总体上表现为毛竹纯林 > 毛竹–杉木混交林 > 杉木纯林。②初始入渗速率、第1阶段入渗速率和平均入渗速率主要受0 ~ 10 cm土层黏粒含量以及10 ~ 20 cm土层细根(< 2 mm)生物量和土壤容重的影响;第2阶段、第3阶段和稳定入渗速率主要受0 ~ 10 cm土层非毛管孔隙度和细根(< 2 mm)生物量以及10 ~ 20 cm土层细根根长密度影响。③细根(< 2 mm)生物量和根长密度可通过影响土壤非毛管孔隙、容重和黏粒含量间接影响土壤入渗速率。④Kostiakov模型是描述不同林分类型下土壤入渗过程的最佳模型。

    Abstract:

    In this study, the infiltration capacities under three typical forest stand types (moso-bamboo forest, moso-bamboo-fir mixed forest, and fir Forest) in Anji County of Zhejiang Province were measured using a table-top double-ring infiltrometer, and the influence of soil properties and root characteristics on soil infiltration rate was analyzed. The results showed that, 1) the initial (947.7–1 220.5 mm/h), the 1st stage (612.6–751.6 mm/h), the 2nd stage (479.0–591.3 mm/h), the 3rd stage (352.9–433.4 mm/h), the stabilized (272.0–369.0 mm/h), and the average (373.1–498.2 mm/h) infiltration rates increased with intensified degree of bamboo invasion. Except for the initial infiltration rate, the others generally reflected the following pattern: severe invasion (moso-bamboo forest) > moderate invasion (moso-bamboo-fir mixed forest) > no invasion (fir forest). 2) Initial, 1st stage and average infiltration rates were mainly influenced by clay contents in 0–10 cm layer, fine root biomass (< 2mm) and soil bulk density in 10–20 cm layer; 2nd stage, 3rd stage and stable infiltration rates were mainly influenced by non-capillary tube porosity, fine root biomass (< 2 mm) in 0-10 cm layer and fine root long density in 10–20 cm layer. 3) Fine root biomass (< 2 mm) and root length density may indirectly affect soil infiltration rate by influencing soil non-capillary porosity, bulk density and clay content. 4) The Kostiakov model was the best model to describe soil infiltration process in three typical forest stand types.

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郭峰,杨思思,张林,邱朝伟,魏侃俐,郭衍瑞,赵天衡,范长江,齐实.浙江安吉三种典型林分类型下土壤入渗特征及其影响因素[J].土壤,2025,57(4):903-910. GUO Feng, YANG Sisi, ZHANG Lin, QIU Zhaowei, WEI Kanli, GUO Yanrui, ZHAO Tianheng, FAN Changjiang, QI Shi. Soil Infiltration Characteristics and Influential Factors Under Three Typical Forest Stand Types in Anji County of Zhejiang Province[J]. Soils,2025,57(4):903-910

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  • 收稿日期:2024-10-22
  • 最后修改日期:2024-12-03
  • 录用日期:2024-12-10
  • 在线发布日期: 2025-09-18
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