Mo Xue, Chen Fei-Jie, You Chong, Liu Fu-de
School of Environmental Science and Safety Engineering, Tianjin University of Technology, Tianjin 300384, China.
Huan Jing Ke Xue. 2020 Feb 8;41(2):895-904. doi: 10.13227/j.hjkx.201908051.
Soil enzymes play key roles in the construction and succession of coastal wetland communities, while the driving mechanism of their activities under water and salt stress conditions is still unclear. The activities and distributions of sucrase, phosphatase, catalase, and urease in the rhizosphere and non-rhizosphere soils of , , and communities were studied in the Yellow River Delta. Moreover, the changes in soil enzyme activities and their influencing factors during the succession of halophytic plant communities were discussed in combination with changes in the physicochemical properties of soil. The results showed significantly higher soil enzyme activities and soil fertility parameters in the rhizosphere soils of , , and communities than those in the non-rhizosphere soils (<0.05). In the rhizosphere soils, the activities of phosphatase and catalase increased in the order of < < , while they increased in the order of < < for sucrase activity, and < < for urease activity. Further, significant differences were found in the physicochemical properties of rhizosphere soils between different halophyte communities (<0.05), which indicated that plant types and their rhizosphere effects could affect soil enzyme activities and fertility characteristics. Furthermore, a two-way analysis of variance showed that the rhizosphere effect was greater than that of vegetation type. The soil sucrase activity was significantly positively correlated with available potassium (AK), available phosphorus (AP), and ammonium nitrogen (NH-N) (<0.05). Meanwhile, urease activity was significantly positively correlated with total nitrogen (TN), organic matter (SOM), AK, AP, NH-N, and nitrate nitrogen (NO-N) (<0.01). Both of the two enzymes were negatively correlated with soil electrical conductivity (EC) (<0.01). The phosphatase and catalase activities were found to be significantly positively correlated with soil water content (MC), total carbon (TC), TN, total phosphorus (TP), SOM, AK, and NH-N (<0.05). Additionally, parameters of pH, total potassium (TK), and NO-N were also significantly associated with catalase activity. Finally, the redundancy analysis (RDA) revealed that main factors affecting the overall soil enzyme activity were TC (<0.01), SOM (<0.01), MC (<0.01), TN (<0.05), NH-N (<0.05), and EC (<0.05). The findings suggested that soil fertility, water, and salinity are the most influential factors of soil enzyme activity in different halophytic plant communities of the Yellow River Delta.
土壤酶在滨海湿地群落的构建和演替中发挥着关键作用,然而其在水盐胁迫条件下的活性驱动机制仍不明确。本研究在黄河三角洲地区,对碱蓬、柽柳和芦苇群落根际与非根际土壤中蔗糖酶、磷酸酶、过氧化氢酶和脲酶的活性及分布进行了研究。此外,结合土壤理化性质的变化,探讨了盐生植物群落演替过程中土壤酶活性的变化及其影响因素。结果表明,碱蓬、柽柳和芦苇群落根际土壤的土壤酶活性和土壤肥力参数显著高于非根际土壤(P<0.05)。在根际土壤中,磷酸酶和过氧化氢酶活性依次为碱蓬<柽柳<芦苇,蔗糖酶活性依次为芦苇<柽柳<碱蓬,脲酶活性依次为碱蓬<芦苇<柽柳。此外,不同盐生植物群落根际土壤的理化性质存在显著差异(P<0.05),这表明植物类型及其根际效应会影响土壤酶活性和肥力特征。进一步的双因素方差分析表明,根际效应大于植被类型效应。土壤蔗糖酶活性与有效钾(AK)、有效磷(AP)和铵态氮(NH₄-N)显著正相关(P<0.05)。同时,脲酶活性与全氮(TN)、有机质(SOM)、AK、AP、NH₄-N和硝态氮(NO₃-N)显著正相关(P<0.01)。这两种酶均与土壤电导率(EC)呈负相关(P<0.01)。磷酸酶和过氧化氢酶活性与土壤含水量(MC)、总碳(TC)、TN、总磷(TP)、SOM、AK和NH₄-N显著正相关(P<0.05)。此外,pH值、全钾(TK)和NO₃-N参数也与过氧化氢酶活性显著相关。最后,冗余分析(RDA)表明,影响土壤酶总活性的主要因素是TC(P<0.01)、SOM(P<0.01)、MC(P<0.01)、TN(P<0.05)、NH₄-N(P<0.05)和EC(P<0.05)。研究结果表明,土壤肥力、水分和盐分是黄河三角洲不同盐生植物群落中土壤酶活性的最主要影响因素。