中国温带地区不同土地利用条件下蚯蚓和蛭石堆肥的特征及其影响因素

Forests Pub Date : 2024-08-08 DOI:10.3390/f15081389
Li Ma, Ming’an Shao, Yunqiang Wang, Tongchuan Li, Xuanxuan Jing, Kunyu Jia, Yangyang Zhang
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引用次数: 0

摘要

蚯蚓群落通过改变微生物群落的多样性和组成来影响土壤碳和氮的循环,从而提高土壤肥力。研究土壤养分组成和细菌群落随蚯蚓群落自然入侵而发生的变化,可能是探索蚯蚓生态功能和准确评估人工林和耕地中碳和氮矿化的关键。本研究考察了扣木林、核桃林、苹果园、猕猴桃园、黑麦草地和玉米田等六种不同土地利用类型生态系统中五种蚯蚓的群落。其中,宝鸡蚯蚓(d)和黑麦草蚯蚓(Amynthas carnosus planus)是主要的蚯蚓物种。在不同的土地利用类型中,夏季蚯蚓密度为 2 至 27 ind-m-2,春季为 15 至 40 ind-m-2。然而,夏季的地表蚯蚓堆肥重量(296.7 至 766.0 g-m-2)大于春季。同一季节的蛭肥重量与蚯蚓数量呈正相关。蛭石堆肥的土壤碳(C)和全氮(N)含量分别为 5.12 至 20.93 g-kg-1 和 0.52 至 1.35 g-kg-1。与土壤相比,蛭石堆肥的碳和氮含量分别增加了 2.0 至 4.3 倍和 1.6 至 7.7 倍。蛭石堆肥的平均 C/N 值(9.5~23.5)高于土壤(7.3~19.8)。由于玉米田和猕猴桃园的土壤中 C 和 N 丰度较高,蚯蚓数量较多,蚯蚓堆肥也较多,因此蚯蚓堆肥的 C 和 N 以及 C/N 均高于土壤。蚯蚓堆肥中的 C 和 N 是通过蚯蚓的排泄和取食活动而不是植被积累的。蚯蚓群落结构在减少细菌多样性、增加蛭堆肥中的蛋白细菌、放线菌、酸性细菌、类杆菌和绿僵菌方面发挥了关键作用,从而丰富了土壤中的 C 和 N 含量,提高了蛭堆肥中的 C/N 含量。因此,今后应更多地关注不同植被生态系统在土壤碳、氮库积累和矿化过程中对蚯蚓群落功能的评价。
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The Characteristics and Influential Factors of Earthworm and Vermicompost under Different Land Use in a Temperate Area, China
Earthworm communities influence soil carbon and nitrogen circulation by altering the diversity and composition of microbial communities, which improves soil fertility. Studying the soil nutrient composition and bacterial communities change in response to earthworm community natural invasion may be key to exploring earthworm ecological functions and accurately assessing C and N mineralization in artificial forests and croplands. In this study, we examined the communities of five earthworm species in ecosystems characterized by six different land-use types, such as buttonwood forest, walnut forest, apple orchard, kiwi orchard, ryegrass land, and corn field. The Metaphire baojiensis (d) and Amynthas carnosus planus were dominant earthworm species. Among different land-use types, earthworm densities ranged from 2 to 27 ind·m−2 in summer and 15 to 40 ind·m−2 in spring. However, surface vermicompost weight in summer (296.7 to 766.0 g·m−2) was greater than in spring. There was a positive correlation between the weight of the vermicompost and earthworm numbers in the same season. Soil carbon (C) and total nitrogen (N) of vermicompost ranged from 5.12 to 20.93 g·kg−1 and from 0.52 to 1.35 g·kg−1, respectively. Compared with soil, the contents of vermicompost C and N increased 2.0 to 4.3 times and 1.6 to 7.7 times, respectively. The average C/N of vermicompost (9.5~23.5) was higher than in the soil (7.3~19.8). Due to the higher abundances of C and N in the soil of corn fields and kiwi orchards, which cultivate higher abundances of earthworms and more vermicompost, the C and N and C/N of vermicompost is higher than in the soil. C and N were accumulated by earthworms’ excreting and feeding activity instead of vegetation in vermicompost. Earthworm community structure plays key roles in decreasing bacterial diversity and adding Proteobacteria, Actinobacteria, Acidobacteria, Bacteroidetes, and Chloroflex in vermicompost, resulting in enriching soil C and N content and increasing C/N in vermicompost. Therefore, the evaluation of different vegetation ecosystems in soil C and N pool accumulation and mineralization should be given more attention regarding the function of earthworm communities in the future.
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