Huang Jun-Jie, Wang Chao, Fang Bo, Feng Lei, Fang Fang, Li Zhe, Guo Jin-Song
College of Urban Construction & Environmental Engineering, Chongqing University, Chongqing 400045, China.
Chongqing Institute of Green and Intelligent Technology, Chinese Academy of Sciences, Chongqing 401122, China.
Huan Jing Ke Xue. 2017 Sep 8;38(9):3673-3681. doi: 10.13227/j.hjkx.201702204.
The concentrations of phosphorus fractions in the soils of the water-level-fluctuating zone (WLFZ) of Pengxi River in the Three Gorges Reservoir were analyzed. The total phosphorus (TP), inorganic phosphorus (IP), and organic phosphorus (OP) were studied using the standard measurement and test (SMT) procedure. The average TP concentration was 575.29 mg·kg and the average OP concentration was 91.23 mg·kg in the soils of WLFZ. The fractions of phosphorus were analyzed by the Hedley method. In the soils of WLFZ, the relative abundance of WA-P (weakly adsorbed inorganic phosphorus), PA-P(potential active inorganic phosphorus), and Fe/Al-P(Fe/Al-bound inorganic phosphorus) accounted for 11.61% of the extractable P, lower than that in the unflooded bankside soils. The relative abundance of WA-P (weakly adsorbed organic phosphorus) and PA-P (potential active organic phosphorus) accounted for 22.28% of the extractable P and the Fe/Al-P (Fe/Al-bound organic phosphorus) accounted for 66.30%. In addition, the P content of the soils of WLFZ was lower than that of the unflooded bankside soils and the difference in the Fe/Al-P content in both soil types was the highest. WA-P and PA-P were significantly correlated with TP in the soils of WLFZ, which indicated that the active phosphorus content was mainly affected by TP. There was no statistical correlation between different fractions of phosphorus, suggesting different sources of phosphorus fractions. The Fe/Al-P content was significantly correlated with OM, implying that the OM content may affect the Fe/Al-P content. Therefore, under flood conditions, the potential impacts of phosphorus in the soils of WLFZ on overlying water should not be neglected.
对三峡水库蓬溪河消落带土壤中的磷组分浓度进行了分析。采用标准测量与试验(SMT)程序研究了总磷(TP)、无机磷(IP)和有机磷(OP)。消落带土壤中TP平均浓度为575.29mg·kg,OP平均浓度为91.23mg·kg。采用Hedley法分析磷的组分。在消落带土壤中,弱吸附无机磷(WA-P)、潜在活性无机磷(PA-P)和铁/铝结合无机磷(Fe/Al-P)的相对丰度占可提取磷的11.61%,低于未淹水的岸边土壤。弱吸附有机磷(WA-P)和潜在活性有机磷(PA-P)的相对丰度占可提取磷的22.28%,铁/铝结合有机磷(Fe/Al-P)占66.30%。此外,消落带土壤的磷含量低于未淹水的岸边土壤,两种土壤类型中铁/铝结合磷含量的差异最大。消落带土壤中WA-P和PA-P与TP显著相关,表明活性磷含量主要受TP影响。不同磷组分之间无统计学相关性,表明磷组分来源不同。铁/铝结合磷含量与有机质(OM)显著相关,意味着OM含量可能影响铁/铝结合磷含量。因此,在洪水条件下,消落带土壤中磷对上覆水体的潜在影响不容忽视。