Chao Jian-Ying, Gao Guang, Tang Xiang-Ming, Dai Jiang-Yu, Zhuang Wei, Zhang Yi-Min
Nanjing Institute of Environmental Science, Ministry of Environmental Protection, Nanjing 210042, China.
Huan Jing Ke Xue. 2011 Oct;32(10):2861-7.
The physical and chemical characteristics were continually monitored during a wind course one time per day, which continued for 10 days, and other water physical and chemical parameters were concomitantly monitored. Organic aggregates (OA) abundance was significantly higher during wind period than calm stage and the maximum of OA abundance, which occurred the same day when wind speed was highest, was 29 times higher than that in the calm stage. Although OA-C, OA-N and OA-P concentration were decreased during wind period, the total C, N and P contend in OA were increased for the increased OA abundance. Additionally, suspended soil (SS), total nitrogen (TN) and total phosphorus (TP) concentration during wind period were significantly higher than that of clam stage, but total dissolved phosphorus (TDP), total dissolved nitrogen (TDN) and soluble reactive phosphorus (SRP) were insignificantly different. During the wind, OA alkaline phosphatase activity (OA-APA) and OA enzymatically hydrolyzable phosphorus (OA-EHP) both increased significantly, which accelerated organic phosphorous mineralization and SRP release. The results indicate that SRP release induced by wind in shallow lakes may comes from suspended matter, especially OA release rather than directly comes from sediment.
在一次为期10天的风程中,每天对物理和化学特征进行一次监测,并同时监测其他水体物理和化学参数。风期有机聚集体(OA)丰度显著高于平静期,且OA丰度最大值出现在风速最高的同一天,比平静期高29倍。虽然风期OA-C、OA-N和OA-P浓度降低,但由于OA丰度增加,OA中的总C、N和P含量增加。此外,风期悬浮土壤(SS)、总氮(TN)和总磷(TP)浓度显著高于平静期,但总溶解磷(TDP)、总溶解氮(TDN)和可溶性活性磷(SRP)无显著差异。在有风期间,OA碱性磷酸酶活性(OA-APA)和OA酶促水解磷(OA-EHP)均显著增加,加速了有机磷矿化和SRP释放。结果表明,浅水湖泊中风诱导的SRP释放可能来自悬浮物,尤其是OA释放,而非直接来自沉积物。