Isaac Yagle , Alon Levinzon , José M. Grünzweig , Jean Marc Dufour-Dror , Udi Zurgil , Vasily I. Grabovsky , Alexandra N. Kravchenko , Ilya Gelfand
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To fill this knowledge gap, we quantified the <em>in-situ</em> soil trace gas emissions and the potential microbial activity in soils under invasive mesquite (<em>Prosopis juliflora</em>) trees (Prosopis), native acacia (<em>Acacia tortilis</em>) trees (Acacia), and in unvegetated soil between trees (Bare soil) on the western shore of the Dead Sea. To account for contributions of spatial and weather variabilities to the emission processes we conducted measurements across two geographic sites, 45 km apart, over two years, both under naturally dry soil conditions and after soil wetting. Before wetting, soil emissions of carbon dioxide (CO<sub>2</sub>) and nitric oxide (NOx) followed the order: Acacia > Prosopis ≥ Bare soil, while soil nitrous oxide (N<sub>2</sub>O) emissions were low and uniform across the three habitats. The soil inorganic N concentration, microbial biomass, and water-extractable organic C were significantly higher under the <em>A</em>. <em>tortilis</em> canopies compared with <em>P</em>. <em>juliflora</em> and Bare soil. After wetting, soil trace gases emissions increased up to 66, 1534, and 42 times, for CO<sub>2</sub>, N<sub>2</sub>O, and NOx, respectively, and remained higher under the native <em>A</em>. <em>tortilis</em> than under <em>P</em>. <em>juliflora</em> and Bare soil (Acacia > Prosopis > Bare soil). The potential soil microbial activity, however, was similar between the soils under the tree canopies. Our results show that the establishment of invasive leguminous trees increase soil CO<sub>2</sub> and gaseous N emissions relative to the Bare soils, but not relative to native leguminous trees.</p></div>","PeriodicalId":21888,"journal":{"name":"Soil Biology & Biochemistry","volume":"198 ","pages":"Article 109558"},"PeriodicalIF":9.8000,"publicationDate":"2024-08-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Invasion of Prosopis trees into arid ecosystem alters soil carbon and nitrogen processes and soil trace gases emissions\",\"authors\":\"Isaac Yagle , Alon Levinzon , José M. Grünzweig , Jean Marc Dufour-Dror , Udi Zurgil , Vasily I. Grabovsky , Alexandra N. 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To account for contributions of spatial and weather variabilities to the emission processes we conducted measurements across two geographic sites, 45 km apart, over two years, both under naturally dry soil conditions and after soil wetting. Before wetting, soil emissions of carbon dioxide (CO<sub>2</sub>) and nitric oxide (NOx) followed the order: Acacia > Prosopis ≥ Bare soil, while soil nitrous oxide (N<sub>2</sub>O) emissions were low and uniform across the three habitats. The soil inorganic N concentration, microbial biomass, and water-extractable organic C were significantly higher under the <em>A</em>. <em>tortilis</em> canopies compared with <em>P</em>. <em>juliflora</em> and Bare soil. After wetting, soil trace gases emissions increased up to 66, 1534, and 42 times, for CO<sub>2</sub>, N<sub>2</sub>O, and NOx, respectively, and remained higher under the native <em>A</em>. <em>tortilis</em> than under <em>P</em>. <em>juliflora</em> and Bare soil (Acacia > Prosopis > Bare soil). 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引用次数: 0
摘要
豆科植物介壳虫(Prosopis spp.)对旱地的入侵往往与土壤有机碳(C)和氮(N)库的增加有关。这些增加刺激了土壤微生物的活动,加速了土壤碳和氮的循环。然而,在一个已有固氮植物种群的生态系统中,介壳虫入侵对土壤生物地球化学的影响,尤其是对痕量气体排放的影响,还没有得到很好的研究。为了填补这一知识空白,我们对死海西岸入侵介壳虫(Prosopis juliflora)树(Prosopis)下的土壤、本地刺槐(Acacia tortilis)树(刺槐)下的土壤以及树与树之间未植被的土壤(裸土)中的原位土壤痕量气体排放和潜在微生物活动进行了量化。为了考虑空间和天气变化对排放过程的影响,我们在相距 45 公里的两个地点进行了为期两年的测量,包括自然干燥土壤条件下和土壤湿润后。在土壤湿润之前,土壤中二氧化碳(CO2)和一氧化氮(NOx)的排放顺序如下相思树 > 槐树 ≥ 裸土,而三种生境的土壤一氧化二氮(N2O)排放量较低且一致。相思树树冠下的土壤无机氮浓度、微生物生物量和水提取有机碳含量明显高于糙叶金合欢和裸土。湿润后,土壤痕量气体排放量(CO2、N2O 和 NOx)分别增加了 66 倍、1534 倍和 42 倍,并且在原生 A. tortilis 树冠下仍然高于 P. juliflora 和裸土(Acacia > Prosopis > Bare soil)。不过,树冠下土壤的潜在土壤微生物活性相似。我们的研究结果表明,与裸土相比,外来入侵豆科树木会增加土壤中的二氧化碳和气态氮排放量,但与本地豆科树木相比则不会。
Invasion of Prosopis trees into arid ecosystem alters soil carbon and nitrogen processes and soil trace gases emissions
The invasion of drylands by leguminous mesquite (Prosopis spp.) is frequently associated with increases in the soil organic carbon (C) and nitrogen (N) pools. These increases stimulate soil microbial activity and accelerate soil C and N cycling. However, the impact of mesquite invasion on soil biogeochemistry, especially the emission of trace gases, in an ecosystem with an already established population of N-fixing plants is not well studied. To fill this knowledge gap, we quantified the in-situ soil trace gas emissions and the potential microbial activity in soils under invasive mesquite (Prosopis juliflora) trees (Prosopis), native acacia (Acacia tortilis) trees (Acacia), and in unvegetated soil between trees (Bare soil) on the western shore of the Dead Sea. To account for contributions of spatial and weather variabilities to the emission processes we conducted measurements across two geographic sites, 45 km apart, over two years, both under naturally dry soil conditions and after soil wetting. Before wetting, soil emissions of carbon dioxide (CO2) and nitric oxide (NOx) followed the order: Acacia > Prosopis ≥ Bare soil, while soil nitrous oxide (N2O) emissions were low and uniform across the three habitats. The soil inorganic N concentration, microbial biomass, and water-extractable organic C were significantly higher under the A. tortilis canopies compared with P. juliflora and Bare soil. After wetting, soil trace gases emissions increased up to 66, 1534, and 42 times, for CO2, N2O, and NOx, respectively, and remained higher under the native A. tortilis than under P. juliflora and Bare soil (Acacia > Prosopis > Bare soil). The potential soil microbial activity, however, was similar between the soils under the tree canopies. Our results show that the establishment of invasive leguminous trees increase soil CO2 and gaseous N emissions relative to the Bare soils, but not relative to native leguminous trees.
期刊介绍:
Soil Biology & Biochemistry publishes original research articles of international significance focusing on biological processes in soil and their applications to soil and environmental quality. Major topics include the ecology and biochemical processes of soil organisms, their effects on the environment, and interactions with plants. The journal also welcomes state-of-the-art reviews and discussions on contemporary research in soil biology and biochemistry.