Institute of Polar Environment, School of Earth and Space Sciences, University of Science and Technology of China, Hefei city, Anhui Province 230026, PR China.
Sci Total Environ. 2011 Sep 1;409(19):3789-800. doi: 10.1016/j.scitotenv.2011.06.034. Epub 2011 Jul 16.
Phosphine (PH(3)), a reduced phosphorus compound, is a highly toxic and reactive atmospheric trace gas. In this study, a total of ten ornithogenic soil/sediment profiles were collected from tundra ecosystems of east Antarctica and Arctic, and matrix-bound phosphine (MBP), the phosphorus fractions and alkaline phosphatase activity (APA) were analyzed. High MBP concentrations were found in these profiles with the range from 39.59 ng kg(-1) dw to 11.77 μg kg(-1) dw. MBP showed a consistent vertical distribution pattern in almost all the soil profiles, and its concentrations increased at soil surface layers and then decreased with depths. MBP levels in the ornithogenic soils were two to three orders of magnitude lower than those in ornithogenic sediments. The yield of PH(3) as a fraction of total P in all the profiles ranged from 10(-5) to 10(-9) mgPH(3) mg(-1)P with higher mean PH(3) yield in the ornithogenic sediments. The ornithogenic soils showed high concentrations of total phosphorus (TP), organic phosphorus (OP), inorganic phosphorus (IP) and metal elements (Cu, Zn, Mn, Fe, Al and Ca) but low MBP levels, vice versa for the ornithogenic sediments. No correlation had been obtained between MBP concentrations and IP, OP and TP. There existed an exponential correlation (r=0.67, p<0.01) between MBP and soil/sediment moisture. MBP concentrations showed a significant positive correlation with APA (r=0.668, p<0.0001), total organic carbon (r=0.501, p<0.0001), total hydrogen (r=0.483, p<0.0001) and total sulfur (r=0.398, p<0.001), indicating that the production of MBP is associated with microbially mediated factors rather than the contents of TP, IP and OP in the P-enriched ornithogenic soils/sediments. Our results indicated that MBP is an important gaseous link in the phosphorus biogeochemical cycles of ornithogenic tundra ecosystems in Antarctica and Arctic.
磷化氢(PH(3))是一种还原态的磷化合物,是一种剧毒且具有强反应活性的痕量气体。本研究共采集了来自东南极和北极地区冻原生态系统的 10 个鸟粪土/沉积物剖面,分析了其中的总结合态磷(MBP)、磷形态和碱性磷酸酶活性(APA)。这些剖面中均检测到高浓度的 MBP,范围为 39.59ngkg(-1)dw 至 11.77μgkg(-1)dw。MBP 在几乎所有土壤剖面上均呈现出一致的垂直分布模式,其浓度在表层土壤中增加,然后随深度降低。鸟粪土中的 MBP 水平比鸟粪沉积物低 2 至 3 个数量级。所有剖面中,总磷(TP)中 PH(3)的释放量占比范围为 10(-5)至 10(-9)mgPH(3)mg(-1)P,鸟粪沉积物中 PH(3)的释放量均值更高。鸟粪土具有较高的总磷(TP)、有机磷(OP)、无机磷(IP)和金属元素(Cu、Zn、Mn、Fe、Al 和 Ca)浓度,但 MBP 水平较低,而鸟粪沉积物则相反。MBP 浓度与 IP、OP 和 TP 之间未呈现相关性。MBP 浓度与土壤/沉积物水分之间存在指数相关性(r=0.67,p<0.01)。MBP 浓度与 APA(r=0.668,p<0.0001)、总有机碳(r=0.501,p<0.0001)、总氢(r=0.483,p<0.0001)和总硫(r=0.398,p<0.001)呈显著正相关,表明 MBP 的产生与微生物介导的因素有关,而与富含磷的鸟粪土/沉积物中的 TP、IP 和 OP 含量无关。本研究结果表明,MBP 是南极和北极地区鸟粪冻原生态系统磷生物地球化学循环中的一个重要气态联系。