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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Spatial distribution characteristics of organic matter and total nitrogen of marsh soils in river marginal wetlands.
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Spatial distribution characteristics of organic matter and total nitrogen of marsh soils in river marginal wetlands.

机译:河流边缘湿地沼泽土壤有机质和全氮的空间分布特征

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摘要

Contents of soil organic matter (SOM) and total nitrogen (TN) in the surface soils and subsurface soils were measured in five types of floodplains classified with different flood frequencies in river marginal wetlands of Erbaifangzi, China, in 1999. Contour maps and profile maps were constructed to describe the spatial distribution of SOM and TN in order to identify the influences of flood frequency on them. Results showed that spatial distributions of both SOM and TN were very similar in soil profiles (0-120 cm) of the five areas, decreasing gradually with depth except an accumulation peak in the flooded floodplain (B area). Also, the accumulation peak in the soil profile of B area was relevant to water table, nitrogen leaching, denitrification and mineralization. However, their horizontal distributions in surface soils (0-10 cm) were different in the five areas. Although the flood could bring the deposit of nutrients and sands, the highest content of SOM or TN did not appear in B area but in the floodplain with certain flood frequency. For example, SOM content (6.76%) in 5-year floodplain wetland was highest, and the highest content of TN (3666.4 mg/kg) appeared in 1-year floodplain wetland. However, SOM and TN contents in soils of B area were 4.08% and 2605.4 mg/kg, respectively. Soil clay content, wetland plant (Phragmites australis) litter inputs, soil moisture and water table greatly affected the spatial distribution of SOM and TN in floodplain wetlands. The ratios of carbon to nitrogen of wetland soils in this region were relatively lower than those in paddy soils. SOM and TN contents were significantly correlated with total phosphorus (TP) contents in floodplain wetlands except the 100-year floodplain wetland, but they were significantly influenced by soil pH values only in B area. Denitrification and ammonia volatilization were the main mechanisms resulting in nitrogen loss of surface soils in B area. Flood frequency significantly influenced the ecological functions such as nutrient retention and water quality maintenance of floodplains.
机译:在1999年中国二百方子河边缘湿地中,以不同洪水频率分类的五种类型的滩涂,测量了表层土壤和地下土壤中的有机质(SOM)和总氮(TN)含量。等高线图和剖面图构造描述SOM和TN的空间分布,以识别洪水频率对其的影响。结果表明,在五个地区的土壤剖面(0-120厘米)中,SOM和TN的空间分布非常相似,除了淹没的洪泛区(B地区)的蓄积峰外,随着深度的增加而逐渐减小。另外,B区土壤剖面中的累积峰与地下水位,氮淋失,反硝化和矿化有关。但是,这五个地区在表层土壤(0-10厘米)中的水平分布是不同的。尽管洪灾可能带来养分和沙粒的沉积,但最高的SOM或TN含量并没有出现在B区,而是以一定的洪灾频率出现在洪泛区。例如,5年洪泛区湿地中的SOM含量最高(6.76%),而1年洪泛区湿地中的TN含量最高(3666.4 mg / kg)。但是,B区土壤的SOM和TN含量分别为4.08%和2605.4 mg / kg。土壤黏土含量,湿地植物(Phragmites australis)凋落物输入,土壤水分和地下水位极大地影响了洪泛区湿地中SOM和TN的空间分布。该地区湿地土壤的碳氮比相对低于水稻土。除100年洪泛区湿地外,洪泛区湿地中SOM和TN含量与总磷(TP)含量显着相关,但仅在B地区,它们受土壤pH值显着影响。反硝化和氨气挥发是造成B区表层土壤氮素流失的主要机理。洪水频率显着影响了洪泛区的养分保留和水质维持等生态功能。

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