黄土丘陵区生物结皮对退耕地土壤质量的影响
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作者单位:

(1.西北农林科技大学资源环境学院,陕西 咸阳 712100;2.中国科学院水利部水土保持研究所,水土保持与荒漠化整治全国重点实验室,陕西 咸阳 712100;3.西北农林科技大学水土保持科学与工程学院,陕西 咸阳 712100)

作者简介:

付立桥(2000-),硕士研究生,研究方向为生物结皮生态功能。E-mail:2163390582@qq.com。

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基金项目:

基金项目:国家自然科学基金(42377357)。


Effects of biological soil crusts on soil quality of abandoned farmland in hilly Loess Plateau region
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(1.College of Natural Resources and Environment,Northwest A & F University,Xianyang Shaanxi 712100;2.Institute of Soil and Water Conservation,Chinese Academy of Sciences and Ministry of Water Resources,State Key Laboratory of Soil and Water Conservation and Desertification Control,Xianyang Shaanxi 712100;3.College of Soil and Water Conservation and Engineering,Northwest A & F University,Xianyang Shaanxi 712100)

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    摘要:

    生物结皮在黄土丘陵区广泛发育,显著影响0~10 cm土壤物理、化学及生物学属性。为明确不同发育年限的生物结皮对土壤质量的影响,利用土壤质量指数(SQI)综合评价该区发育年限为1~30年的生物结皮及其下层0~2、2~5、5~10 cm土层土壤质量,采用主成分及相关性分析确定了生物结皮改善土壤质量的关键因子。结果表明:(1)随着发育年限的增加,生物结皮层及下层土壤物理、化学及生物学属性明显改善。生物结皮降低了土壤容重,提高了土壤田间持水量、总孔隙度和磷酸酶活性,提升了土壤有机质、全氮、全磷、有效磷含量。(2)生物结皮对土壤质量的提升作用随着土层深度的增加而降低。相同年限下,生物结皮层与0~2 cm土层SQI相差0.11~0.30,而0~2与5~10 cm土层SQI相差0.03~0.06。(3)生物结皮对土壤质量的改善与其发育年限有关。生物结皮层SQI在其发育前3年提升至0.64,0~2 cm土层SQI在生物结皮发育前5年提升至0.56,较撂荒地提高了48.82%;生物结皮层、0~2 cm土层SQI均在第13年左右达到最高值,分别为0.85和0.67,而后趋于稳定。(4)土壤有机质和全氮含量的提高是生物结皮改善土壤质量的关键因子。研究明确了不同发育年限的生物结皮对土壤质量的综合影响,强化了生物结皮生态功能认识。

    Abstract:

    Biological soil crusts is widely developed in hilly Loess Plateau region,which significantly affects the soil physical,chemical and biological properties of 0-10 cm soil layer. To clarify the comprehensive effect of biological soil crusts of varying developmental ages on soil quality,the soil quality index(SQI)was employed in this study to evaluate the effects of biological soil crusts aged 1 to 30 years on soil quality across different layers,specifically the biological soil crusts layer,namely,0–2,2–5 and 5–10 cm. Principal component and correlation analysis were utilized to identify the key factors of improving soil quality. The results showed that:(1)With the increase of development years,the physical,chemical and biological properties of biological soil crusts layer and subsoil layer were obviously improved. Biological crust decreased soil bulk density,increased soil field water capacity,total porosity and phosphatase content,and increased soil organic matter,total nitrogen,total phosphorus and available phosphorus contents.(2)The improvement of soil quality by biological soil crusts decreased with increasing soil layer depth. Within the same year,the difference between SQI of biological soil crusts layer and 0–2 cm soil layer ranged from 0.11 to 0.30,while the difference between 0–2 and 5–10 cm soil layers was only 0.03 to 0.06.(3)The improvement of soil quality by biological soil crusts was related to the years of development. The SQI of the biological soil crusts reached 0.64 within the first three years of development,and the SQI of 0–2 cm soil layer increased to 0.56 in the first five years of biological soil crusts development,which was 48.82% higher than that of abandoned land. The SQI of biological soil crusts layer and 0–2 cm soil layer reached the highest values around the 13th year,which was 0.85 and 0.67,respectively,and then tended to stabilize.(4)Soil organic matter and total nitrogen content were the key factors that improve soil quality through biological soil crusts. This study clarified the comprehensive effect of biological soil crusts of varying ages on soil quality,and strengthened the understanding of ecological function of biological soil crusts.

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付立桥,赵允格,高丽倩,乔羽.黄土丘陵区生物结皮对退耕地土壤质量的影响[J].中国土壤与肥料,2025,(4):1-9.

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  • 收稿日期:2024-08-02
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  • 录用日期:2024-12-16
  • 在线发布日期: 2025-06-25
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