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应用生态学报 ›› 2022, Vol. 33 ›› Issue (11): 3046-3054.doi: 10.13287/j.1001-9332.202211.015

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冀北土石山区不同土地利用类型土壤质量评价

滕慧颖1, 耿艳楼1, 张恒硕2, 查同刚2*   

  1. 1国家半干旱农业工程技术研究中心, 石家庄 050051;
    2北京林业大学水土保持学院, 北京 100083
  • 收稿日期:2021-11-15 修回日期:2022-08-31 出版日期:2022-11-15 发布日期:2023-05-15
  • 通讯作者: *E-mail: zhtg73@bjfu.edu.cn
  • 作者简介:滕慧颖, 女, 1969年生, 正高级工程师。主要从事林业工程和生态修复研究。E-mail: hyhy07@126.com
  • 基金资助:
    冬奥赛区植物景观提升关键技术集成示范项目(20476801D)

Assessment of soil quality under different land use types in the rocky mountain area of northern Hebei Province, China.

TENG Hui-ying1, GENG Yan-lou1, ZHANG Heng-shuo2, ZHA Tong-gang2*   

  1. 1National Semi-arid Agriculture Engineering and Technology Research Center of China, Shijiazhuang 050051, China;
    2School of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China
  • Received:2021-11-15 Revised:2022-08-31 Online:2022-11-15 Published:2023-05-15

摘要: 为防止北方土石山区的土地和植被在人类活动下进一步退化,为冬奥会赛后制定战略性植被恢复计划,以白桦天然林、落叶松人工林、天然灌草地和弃耕农地为研究对象,基于土壤容重、孔隙度和土壤养分含量等13种土壤理化指标,对冀北土石山区不同土地利用类型土壤质量进行综合评价。结果表明: 冀北土石山区不同土地利用类型土壤质量呈现出白桦天然林>天然灌草地>落叶松人工林>弃耕农地。白桦天然林的土壤质量显著高于其他3种土地利用类型,其土壤全氮(3.24±1.42 g·kg-1)和全磷(0.59±0.10 g·kg-1)含量较高,土壤养分的长期积累是阻止白桦天然林土壤退化的最主要原因;天然灌草地受到土壤粗粒含量和地形因素的影响,土壤质量仅次于白桦天然林;经过40年植被恢复的落叶松人工林土壤物理性质得到改良,土壤砾石含量显著降低,而土壤养分指标未发生显著变化;弃耕农田土壤质量最低的主要原因是植被覆盖低及低海拔区域较高的人类活动强度。受土壤全氮含量的影响,4种土地利用类型下的土壤质量随海拔升高而增加,且均在1700 m左右达到峰值。综上,建议加强在低海拔生态脆弱区域的封禁管理和生态恢复措施,同时兼顾高密度林分的可持续发展,增强人工林的生态适应性。

关键词: 土壤质量, 土石山区, 空间分布, 土地利用类型

Abstract: To assess the variations of soil quality among land use types and with altitude in the rocky mountain area of northern Hebei Province is critical for preventing further human-induced degradation of land and vegetation, and for formulating a strategic plan on vegetation restoration after the Beijing Winter Olympics. Taking Betula platyphylla natural forest, Larix gmelinii plantation, natural grassland and abandoned cropland as research objects, 13 soil physicochemical indices (e.g., soil bulk density, porosity and soil nutrient content) were measured to compare soil quality among land use types. The results showed that soil quality presented the trend as B. platyphylla natural forest > natural grassland > L. gmelinii plantation > abandoned cropland. B. platyphylla natural forest had the best soil quality due to high total nitrogen (3.24 ±1.42 g·kg-1) and phosphorus (0.59±0.10 g·kg-1) contents, suggesting that long-term soil nutrient accumulation played an important role in preventing soil degradation. Soil quality in natural grassland was lower than that in B. platyphylla natural forest, due to topographic factors and coarse soil fraction. Soil physical properties in L. gmelinii plantation had been substantially improved after 40 years restoration, as indicated by significant reductions in soil gravel fraction, while soil nutrient contents changed little. The low soil quality in abandoned cropland was attributable to low vegetation coverage and intense human activities in the low-altitude area. Driven by soil total nitrogen, soil quality under the four land use types increased with altitude, and peaked at about 1700 m. We suggested that enclosure and ecological restoration measures should be strengthened in ecologically-fragile, low-altitude areas, taking sustainable development into consideration for high-density stands and promoting plantations to adapt to environmental change.

Key words: soil quality, mountainous area, spatial distribution, land use type