Leilei Ding, Hong Chen, Xin Wei, Taoying Qin, Xia Lei, Jingyi Li, Yujun Zhang, Lili Zhao, Puchang Wang
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Compared with no grazing, grazing remarkably declined the 0-5 cm soil AP by 73.10% ( p = 0.0250), the 0-5, 5-10, 10-20 cm soil WC by 47.19% ( p = 0.0042), 37.19% ( p = 0.0090), and 30.80% ( p = 0.0034), however, grazing remarkably increased the 0-5, 5-10, 10-20, 20-30 cm soil ACa by 188.76% ( p = 7.9e-05), 93.24% ( p = 0.0177) ,84.18% ( p = 0.00067), and 38.77% ( p = 0.01368), the 0-5, 5-10 cm soil AMg by 186.69% ( p = 0.0016), 78.89% ( p = 0.0109), the 0-5, 5-10, 10-20 cm soil pH by 0.51 ( p = 0.0013), 0.37 ( p = 0.0006), and 0.27 ( p = 0.0114) units, the 0-5, 5-10, 10-20 cm soil BD by 59.03% ( p = 0.0077), 44.14% ( p = 0.0147), and 35.55% ( p = 0.0071), the 30-50 cm soil WC by 22.88% ( p = 0.0241), the 0-5 cm soil βGC by 89.49% ( p = 0.0011), the 0-5, 5-10 cm soil ACP by 7.87% ( p = 0.0300), 6.57% ( p = 0.0240), respectively. Grazing exacerbated the microbial C limitation of 0-5 and 10-20 cm soils by 20.51% ( p = 0.0078) and 40.38% ( p = 0.0209) and switched the soil microbiome from under N limitation to under P limitation at 5-10 cm ( p = 0.0390). Specific soil available cations were identified as the important factors that significantly explained the variation of soil ecto-enzyme activities and soil microbial carbon and nutrient limitations.","PeriodicalId":510399,"journal":{"name":"Polish Journal of Environmental Studies","volume":"12 8","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-04-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Soil Cations Explain the Variation of Soil\\nExtracellular Activities and Microbial Elemental\\nLimitations on Subtropical Grassland, China\",\"authors\":\"Leilei Ding, Hong Chen, Xin Wei, Taoying Qin, Xia Lei, Jingyi Li, Yujun Zhang, Lili Zhao, Puchang Wang\",\"doi\":\"10.15244/pjoes/176566\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The objective of this study was to compare the effects of grazing and non-grazing on the physicochemical properties, stoichiometry, ecto-enzyme activities, and microbial element limitations of soils at five depths in subtropical grassland, China, and to identify the influencing factors of enzyme activities and element limitations. Results showed that grazing, soil depth, and the interaction between grazing and depth remarkably changed soil available phosphorus (AP), available potassium (AK), available calcium (ACa) and available magnesium contents (AMg), bulk density (BD), water content (WC), and β-glucosidase activity (βGC) ( p = 6.702e-9 - 0.04739). Compared with no grazing, grazing remarkably declined the 0-5 cm soil AP by 73.10% ( p = 0.0250), the 0-5, 5-10, 10-20 cm soil WC by 47.19% ( p = 0.0042), 37.19% ( p = 0.0090), and 30.80% ( p = 0.0034), however, grazing remarkably increased the 0-5, 5-10, 10-20, 20-30 cm soil ACa by 188.76% ( p = 7.9e-05), 93.24% ( p = 0.0177) ,84.18% ( p = 0.00067), and 38.77% ( p = 0.01368), the 0-5, 5-10 cm soil AMg by 186.69% ( p = 0.0016), 78.89% ( p = 0.0109), the 0-5, 5-10, 10-20 cm soil pH by 0.51 ( p = 0.0013), 0.37 ( p = 0.0006), and 0.27 ( p = 0.0114) units, the 0-5, 5-10, 10-20 cm soil BD by 59.03% ( p = 0.0077), 44.14% ( p = 0.0147), and 35.55% ( p = 0.0071), the 30-50 cm soil WC by 22.88% ( p = 0.0241), the 0-5 cm soil βGC by 89.49% ( p = 0.0011), the 0-5, 5-10 cm soil ACP by 7.87% ( p = 0.0300), 6.57% ( p = 0.0240), respectively. Grazing exacerbated the microbial C limitation of 0-5 and 10-20 cm soils by 20.51% ( p = 0.0078) and 40.38% ( p = 0.0209) and switched the soil microbiome from under N limitation to under P limitation at 5-10 cm ( p = 0.0390). 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引用次数: 0
摘要
本研究旨在比较放牧和非放牧对中国亚热带草原5个深度土壤理化性质、化学计量学、外源酶活性和微生物元素限制的影响,并确定酶活性和元素限制的影响因素。结果表明,放牧、土壤深度以及放牧与土壤深度的交互作用显著改变了土壤可利用磷(AP)、可利用钾(AK)、可利用钙(ACa)和可利用镁(AMg)含量、容重(BD)、含水量(WC)和β-葡萄糖苷酶活性(βGC)(p = 6.702e-9 - 0.04739)。与不放牧相比,放牧显著降低了 0-5 厘米土壤 AP 的 73.10%( p = 0.0250),0-5、5-10、10-20 厘米土壤 WC 的 47.19%( p = 0.0042)、37.19%( p = 0.0090)和 30.80%( p = 0.0034),但放牧显著增加了 0-5、5-10、10-20、20-30 cm 土壤 ACa 188.76%( p = 7.9e-05) 、93.24%( p = 0.0177) 、84.18%( p = 0.00067) 和 38.77%( p = 0.01368),0-5、5-10 cm 土壤 AMg 186.69%( p = 0.0016)、78.89%(p = 0.0109),0-5、5-10、10-20 cm 土壤 pH 值分别降低 0.51(p = 0.0013)、0.37(p = 0.0006)、0.27(p = 0.0114)个单位,0-5、5-10、10-20 cm 土壤 BD 值分别降低 59.03%(p = 0.0077)、44.14%(p = 0.0147) 和 35.55% ( p = 0.0071),30-50 cm 土壤 WC 分别降低 22.88% ( p = 0.0241),0-5 cm 土壤 βGC 降低 89.49% ( p = 0.0011),0-5、5-10 cm 土壤 ACP 分别降低 7.87% ( p = 0.0300)、6.57% ( p = 0.0240)。放牧加剧了 0-5 和 10-20 厘米土壤微生物的 C 限制,分别为 20.51% ( p = 0.0078) 和 40.38% ( p = 0.0209),并使 5-10 厘米土壤微生物群从 N 限制转为 P 限制 ( p = 0.0390)。特定的土壤可利用阳离子被认为是显著解释土壤外切酶活性和土壤微生物碳和养分限制变化的重要因素。
Soil Cations Explain the Variation of Soil
Extracellular Activities and Microbial Elemental
Limitations on Subtropical Grassland, China
The objective of this study was to compare the effects of grazing and non-grazing on the physicochemical properties, stoichiometry, ecto-enzyme activities, and microbial element limitations of soils at five depths in subtropical grassland, China, and to identify the influencing factors of enzyme activities and element limitations. Results showed that grazing, soil depth, and the interaction between grazing and depth remarkably changed soil available phosphorus (AP), available potassium (AK), available calcium (ACa) and available magnesium contents (AMg), bulk density (BD), water content (WC), and β-glucosidase activity (βGC) ( p = 6.702e-9 - 0.04739). Compared with no grazing, grazing remarkably declined the 0-5 cm soil AP by 73.10% ( p = 0.0250), the 0-5, 5-10, 10-20 cm soil WC by 47.19% ( p = 0.0042), 37.19% ( p = 0.0090), and 30.80% ( p = 0.0034), however, grazing remarkably increased the 0-5, 5-10, 10-20, 20-30 cm soil ACa by 188.76% ( p = 7.9e-05), 93.24% ( p = 0.0177) ,84.18% ( p = 0.00067), and 38.77% ( p = 0.01368), the 0-5, 5-10 cm soil AMg by 186.69% ( p = 0.0016), 78.89% ( p = 0.0109), the 0-5, 5-10, 10-20 cm soil pH by 0.51 ( p = 0.0013), 0.37 ( p = 0.0006), and 0.27 ( p = 0.0114) units, the 0-5, 5-10, 10-20 cm soil BD by 59.03% ( p = 0.0077), 44.14% ( p = 0.0147), and 35.55% ( p = 0.0071), the 30-50 cm soil WC by 22.88% ( p = 0.0241), the 0-5 cm soil βGC by 89.49% ( p = 0.0011), the 0-5, 5-10 cm soil ACP by 7.87% ( p = 0.0300), 6.57% ( p = 0.0240), respectively. Grazing exacerbated the microbial C limitation of 0-5 and 10-20 cm soils by 20.51% ( p = 0.0078) and 40.38% ( p = 0.0209) and switched the soil microbiome from under N limitation to under P limitation at 5-10 cm ( p = 0.0390). Specific soil available cations were identified as the important factors that significantly explained the variation of soil ecto-enzyme activities and soil microbial carbon and nutrient limitations.