黄河游荡性河段滩区不同人类干扰程度对水土氮、磷、钾分布的影响

    Effects of different human interference degrees on the distribution of nitrogen, phosphorus and potassium in water and soil in the beach area of the wandering reach of the Yellow River

    • 摘要: 为研究不同人类干扰程度对黄河下游游荡性河段氮(N)、磷(P)、钾(K)含量的影响,采集未受到人类干扰的嫩滩裸地(Ⅰ区)、受人类轻度干扰的高滩农田(Ⅱ区)、受人类高度干扰的大堤内侧农田(Ⅲ区)和干扰恢复区黄河故道(Ⅳ区)的土壤、地表水与地下水样品,分析N、P、K含量特征及相关理化性质。结果表明: ①Ⅰ区和Ⅱ区由于较高的地下水水位与季节性水淹造成土壤物理性质较差,不适宜植被生长,其他区域由于植被的根系作用以及生物、微生物的活动改善了土壤物理性质; ②土壤有机质(soil organic matter, SOM)和全氮(total nitrogen, TN)受黄河渗透影响较大,但Ⅱ区受水流冲刷作用造成二者含量较低,Ⅲ区受人类活动影响总氮相对较高,总磷(total phosphorus, TP)和总钾(total potassium, TK)主要受成土母质影响,仅在Ⅱ区受人类活动影响较大, Ⅰ区土壤主要受P限制,其他区受N限制严重; ③地下水中K、总有机碳(total organic carbon, TOC)和NO3-组分沿地表水侧渗路径表现出明显的空间变化规律,部分地下水样品NH4+、NO3含量超标,地下水组分在受黄河水化学成分影响同时受人类活动影响。研究探讨在地表水—土壤—地下水循环过程中,氮磷钾和人类活动之间的关系,可为黄河下游湿地生态系统保护工作提供科学依据。

       

      Abstract: In order to study the characteristics of nitrogen, phosphorus, and potassium content under different degrees of human interference, the authors collected samples of soil, surface water, and groundwater from non-human-disturbed bare beach (Ⅰ), the high-beach farmland with mild human disturbance (Ⅱ), the farmland inside the levee with great human disturbance (Ⅲ) and the disturbance restoration zone of the old course of the Yellow River(Ⅳ). Nitrogen, phosphorus, potassium, potassium and other related physical and chemical properties were analyzed. The results showed that the soil physical properties in Ⅰ and Ⅱ zones were poor due to the high groundwater level and seasonal flooding, and it was not suitable for vegetation growth. In other zones, soil physical properties were improved due to the root action of vegetation and the activities of organisms and microorganisms. SOM and total nitrogen (TN) were seriously affected by the Yellow River seepage, and their content in Ⅱ zone was low due to the erosion of water flow. The TN content was high in Ⅲ zone due to human activities. TP and TK were mainly affected by the soil parent material, and were greatly affected by human activity in Ⅲ zone. The soil in I zone was mainly limited by P, and the other areas were severely limited by N. K、TOC and NO3- in groundwater exhibit significant spatial variation patterns along the lateral infiltration path of surface water. NH4+ and NO3- content in some groundwater samples exceeded the standard. The composition of groundwater was influenced by both the chemical composition of the Yellow River and human activities. The relationship between N, P, K and human activity was studied during the circulation process of water-soil-groundwater, providing scientific basis for the protection of wetland ecosystem in the lower reaches of the Yellow River.

       

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