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    干湿变化下凋落物分解过程中生态修复边坡土壤酶活性及其化学计量特征研究

    Investigations into Soil Enzyme Activities and their Stoichiometric Characteristics during Litter Decomposition under Varied Moisture Conditions in Ecologically Restored Slopes

    • 摘要: 土壤酶活性的变化能敏锐地指示土壤生物化学过程及其对环境干扰的响应,是评估边坡生态修复效果的有效生物学指标。自然环境中的干湿交替过程显著影响土壤酶活性及其驱动的养分循环,但相关研究仍较薄弱,对人工修复边坡这类特殊生境更是如此。为探讨干湿变化条件下生态修复边坡凋落物分解过程中土壤酶活性及其化学计量特征,提升人工边坡生态系统的稳定性和可持续性,本研究土样取自湖北省宜昌市典型植被混凝土修复边坡,采用室内模拟培养试验,共设置四个田间持水量梯度处理:恒定40%(W1)、恒定70%(W2)、中度干湿变化(W3,60%至20%)和剧烈干湿变化(W4>,100%至35%),并设置5个干湿变化周期和无凋落物对照,测定土壤总有机碳(SOC)、铵态氮(NH₄⁺-N)和速效磷(AP)含量,并分析β-1,4-葡萄糖苷酶(BG)、N-乙酰-β-氨基葡萄糖苷酶(NAG)、亮氨酸氨基肽酶(LAP)、中性磷酸酶(NP)、纤维素酶(CBH)和多酚氧化酶(PPO)的酶活性及其酶化学计量比和矢量特征。土壤SOC和NH₄⁺-N含量均随干湿变化周期进行而下降;SOC在W4水分梯度下降了77.1%,在W1下降了17.8%,干湿变化处理的降幅显著小于恒定水分处理(P<0.05)。本研究中,土壤酶碳氮磷比值多数偏离1:1:1,土壤酶碳氮比最大值为1.23,小于1.41的全球平均值,酶氮磷比最小值为0.59高于全球均值0.44,说明本研究所选的宜昌植被混凝土修复边坡整体上土壤氮元素相对缺乏,且剧烈的干湿变化加剧了土壤氮限制。在W4水分梯度下,有凋落物时矢量角度下降了9.8%,无凋落物时下降了7.4%,有凋落物时下降幅度有所减缓,说明凋落物添加可缓解由干湿变化引起的养分限制。

       

      Abstract: 【Background】Changes in soil enzyme activity can sensitively indicate soil biochemical processes and their responses to environmental disturbances, and is an effective biological indicator for evaluating the effectiveness of slope ecological restoration. Alternating drying and wetting processes in natural environments significantly affect soil enzyme activity and the nutrient cycling driven by it, but relevant research remains relatively insufficient, especially for special habitats such as artificially restored slopes. 【Methods】To explore the soil enzyme activities and their chemical stoichiometric characteristics during the decomposition process of litter on ecological restoration slopes under dry-wet conditions, and to enhance the stability and sustainability of artificial slope ecosystems, this study collected soil samples from typical vegetation concrete restoration slopes in Yichang City, Hubei Province. Using indoor simulation cultivation experiments, four field water holding capacity gradient treatments were set up: constant 40% (W1), constant 70% (W2), moderate dry-wet variation (W3, 60% to 20%), and severe dry-wet variation (W4, 100% to 35%). Five dry-wet variation cycles and no litter control were also set up. The contents of total soil organic carbon (SOC), ammonium nitrogen (NH₄⁺-N), and available phosphorus (AP) were determined, and the enzyme activities, enzyme stoichiometric ratios, and vector characteristics of β-1,4-glucosidase (BG), N-acetyl-β-amino-glucosidase (NAG), leucine aminopeptidase (LAP), neutral phosphatase (NP), cellulase (CBH), and polyphenol oxidase (PPO) were analyzed. 【Results】The results showed that the contents of SOC and NH₄⁺-N in the soil decreased with the dry-wet variation cycles. SOC decreased by 77.1% at the W4 water gradient and by 17.8% at W1. The decrease in the dry-wet variation treatments was significantly smaller than that in the constant water treatment (P<0.05). 【Conclusion】In this study, the soil enzyme carbon-nitrogen-phosphorus ratios mostly deviated from 1:1:1. The maximum soil enzyme carbon-nitrogen ratio was 1.23, which was less than the global average of 1.41. The minimum enzyme nitrogen-phosphorus ratio was 0.59, which was higher than the global average of 0.44. This indicates that the selected Yichang vegetation concrete restoration slope overall has a relative deficiency of soil nitrogen elements, and the severe dry-wet variation exacerbated the soil nitrogen limitation. At the W4 water gradient, the vector angle decreased by 9.8% with litter, and by 7.4% without litter. The decrease was slightly slower with the addition of litter, indicating that the addition of litter can alleviate the nutrient limitation caused by dry-wet variations.

       

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