半干旱草原大中型土壤动物在畜粪分解中的作用
收稿日期: 2022-10-10
录用日期: 2022-11-28
网络出版日期: 2022-12-08
基金资助
国家自然科学基金(32071564);国家自然科学基金(41561055);内蒙古自治区科技计划(2019ZD007);内蒙古自治区科技计划(2021ZD0011)
Effects of soil macro- and meso-fauna on the decomposition of cattle and horse dung pats in a semi-arid steppe
Received date: 2022-10-10
Accepted date: 2022-11-28
Online published: 2022-12-08
土壤动物是陆地生态系统的重要组分, 在有机质分解过程中具有重要作用。目前有关土壤动物在生态系统分解中的作用研究主要聚焦于植物凋落物的分解, 而对动物粪便分解的研究稀少。本研究在内蒙古典型草原设置了马粪和牛粪分解原位实验, 使用不同孔径的金属隔离网排除不同体型大小的土壤动物, 通过测定大中型土壤动物对畜粪分解过程中质量损失、碳氮含量和微生物呼吸以及土壤养分动态变化的影响, 解析其在分解中的作用。设置5个处理, 即CK, 仅土壤, 无粪; T0, 粪添加+0.425 mm隔离网(排除了粪居型和掘洞型粪金龟和中型土壤动物); T1, 粪添加+1 mm隔离网(排除了粪居型和掘洞型粪金龟); T2, 粪添加+2 mm隔离网(排除了掘洞型粪金龟); T3, 仅粪添加(不排除土壤动物)。结果表明: (1)在畜粪分解60天内, 土壤动物对畜粪的干质量损失没有显著的促进作用(P > 0.05); 相反, 在畜粪分解360天, 不隔离土壤动物处理(T3)显著地提高了牛粪干质量损失(P < 0.05), 而降低了马粪干质量损失(P < 0.05)。(2)在畜粪分解的60天内, 畜粪中碳和氮含量下降速度在有土壤动物存在的情况下(T3)快于隔离土壤动物(T0和T1)。(3)两种畜粪添加增加了土壤微生物的呼吸, 且这种增加趋势在实验的第15天和第30天在土壤动物存在时(T3)最明显。(4)与对照(CK)相比, 马粪添加处理提高了土壤速效氮、有机碳的含量和土壤含水量, 且这种增加趋势在排除掘洞型粪金龟(T2)和不排除土壤动物(T3)条件下表现更显著(P < 0.05), 而牛粪添加处理没有明显改变这些指标(P > 0.05)。研究表明, 分解初期粪金龟的取食和活动会改变畜粪的理化性质, 进而影响分解后期土壤生物在畜粪分解中的作用。
程建伟 , 王亚东 , 王桠楠 , 李莹 , 郭颖 , 白正 , 刘新民 , 李永宏 . 半干旱草原大中型土壤动物在畜粪分解中的作用[J]. 生物多样性, 2022 , 30(12) : 22575 . DOI: 10.17520/biods.2022575
Aims: Soil fauna as the key component of terrestrial ecosystems, playing an important role in decomposition of animal dung, mineralization of organic matter and turnover of soil nutrients. Many studies have been done on the soil fauna’s effects on plant litter’s decomposition. Still, less information is available on their impact on the decomposition of animal dung.
Methods: Here we conducted a field experiment in a temperate semi-arid steppe ecosystem to investigate the effect of the different soil fauna groups with different body sizes on the decomposition of horse and cattle dung pats on the soil surface over a one-year period. The experiment had five treatments: CK, soil only, no dung nor soil fauna; T0, dung pat covered with a wire-mesh-cage of 0.425 mm holes (excluding dung beetles and soil meso-fauna); T1, dung pat covered with a wire-mesh-cage of 1 mm holes (excluding dung beetles); T2, dung pat covered with a wire-mesh-cage of 2 mm holes (excluding tunneler dung beetle); T3, exposed dung (with no exclusion of soil fauna).
Results: We found that (1) compared with dung only (excluding dung beetles and soil meso-fauna) treatment (T0), the presence of soil fauna (T1, T2 and T3) did not enhance the dry mass loss of livestock dung during the first 60 days of the experiment; in contrast, in the presence of all soil fauna (T3) significantly increased the dry mass loss of cattle dung but decreased that of horse dung at the end of the experiment (at day 360). (2) Soil fauna also enhanced the decline rate of carbon and nitrogen content in dung during the first 60 days of the experiment. (3) Dung addition increased the soil microbial respiration, and the increase was most obvious in the presence of soil fauna (T3) on days 15 and 30 of the experiment. (4) Compared to the soil with no dung (CK), the soil with horse dung had higher contents of soil available N, soil organic carbon and soil moisture, and the contents were higher in the presence of soil fauna (T2 and T3); whereas the soil with cattle dung had no changes.
Conclusion: We conclude that the feeding and activities of dung beetle in the early stage of dung decomposition alter the physicochemical properties of dung, which indirectly affect the role of soil biota in the decomposition in the later stage.
Key words： soil fauna; dung decomposition; nutrient release; microbial activity; geochemistry
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