华西雨屏区常绿阔叶林不同深度土壤氮矿化及酶活性对模拟氮沉降的响应
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国家自然科学基金项目(32071591)


Responses of soil nitrogen mineralization and enzyme activities at different depths to nitrogen additions in an evergreen broad-leaved forest
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National Natural Science Foundation of China (32071591)

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    摘要:

    在森林土壤中,无机氮的垂直移动速率较快,因此大气氮沉降极有可能对下层森林土壤造成较大影响,且表层土壤往往与下层土壤的物理化学特性和所处环境差异较大,因此土壤剖面中不同深度的土壤对大气氮沉降的响应可能存在较大差异。以往研究表明,"华西雨屏"区的年均氮湿沉降量高达95 kg N hm-2 a-1,处于中国最高水平,该森林生态系统出现一定氮饱和特征。基于以上背景,研究华西雨屏区常绿阔叶林不同深度土壤氮矿化及相关酶活性对模拟氮沉降的响应,从2014年1月起进行野外定位模拟氮沉降试验,分别设置对照(CK,+0 g N hm-2 a-1)、低氮(LN,+5 g N hm-2 a-1)和高氮(HN,+15 g N hm-2 a-1)3个氮添加水平。在氮沉降进行5年后进行土壤采样,测定不同深度土壤(上层0-15 cm、中层15-30 cm、下层30-45 cm)全氮(TN)、硝态氮(NO3--N)、铵态氮(NH4+-N)含量及氮矿化相关酶活性。结果表明:(1)该常绿阔叶次生林不同深度土壤TN有显著差异;(2)模拟氮沉降对该系统土壤氮矿化总体表现出极显著抑制作用,其中中层土壤抑制作用最为强烈,净氮矿化速率主要受硝化过程的影响;(3)氮矿化相关酶活性均随土壤深度的加深而降低,模拟氮沉降对土壤脲酶活性有极显著促进作用,对土壤硝酸还原酶活性有显著抑制作用。由于无机氮在土壤剖面中的高度可移动性,深层土壤氮循环和特征对氮沉降的响应需要更加密切的关注。

    Abstract:

    In forest soil, the vertical migration rate of inorganic nitrogen is faster, so atmospheric nitrogen deposition is likely to have a greater impact on the lower forest soil, and the surface soil is often quite different from the lower forest soil in physical chemistry characteristics and environment. Therefore, the response of soil to atmospheric nitrogen deposition at different depths in the soil profile may be quite different. Previous studies have shown that the annual average wet deposition of nitrogen was as high as 95 kg N hm-2 a-1, which is the highest in rainy area of western China. Based on the above background, the responses of soil nitrogen mineralization and related enzyme activities to the simulated nitrogen deposition at different depths in the evergreen broad-leaved forest in rainy area of western China were studied. Three groups were set including control (CK, +0 g N hm-2 a-1), low nitrogen (LN, +5 g N hm-2 a-1), and high nitrogen (HN, +15 g N hm-2 a-1). Total nitrogen (TN), nitrate nitrogen (NO3--N), ammonium nitrogen (NH4+-N) and nitrogen mineralization-related enzyme activities were measured at different depths (upper layer 0-15 cm, middle layer 15-30 cm, lower layer 30-45 cm) of soil after 5 years of nitrogen deposition. The results showed that:(1) there were significant differences in TN at different depths of the evergreen broad-leaved secondary forest; (2) The simulated nitrogen deposition showed a very significant inhibitory effect on soil nitrogen mineralization in the system, especially in the middle layer soil. The net nitrogen mineralization rate was mainly influenced by nitrification process; (3) The simulated nitrogen deposition significantly promoted soil urease activity and inhibited soil nitrate reductase activity. Due to the high mobility of inorganic nitrogen in the soil profile, the response of nitrogen cycling and characteristics to nitrogen deposition in deep soil layers needs more close attention.

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宋思意,吕思扬,邱岭军,王馨逸,涂利华.华西雨屏区常绿阔叶林不同深度土壤氮矿化及酶活性对模拟氮沉降的响应.生态学报,2022,42(22):9045~9056

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