首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >Effects of revetment type on the spatial distribution of soil nitrification and denitrification in adjacent tidal urban riparian zones
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Effects of revetment type on the spatial distribution of soil nitrification and denitrification in adjacent tidal urban riparian zones

机译:护垫型对邻近城市河岸区土壤硝化与反硝化的空间分布的影响

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Revetments between the river channels and riparian zones are important factors in the modification of urban riparian zones structure, particularly in zones adjacent to them. Although there have been many studies on the stability of revetments in tidal urban riparian zones, the quantitative effects of revetments on the nitrogen cycling in riparian zones adjacent to them remain unclear. Tidal riparian zones undergo more frequent river-soil exchanges than normal riparian areas, thus, revetments may have a greater impact on the nitrogen cycling. Nitrification and denitrification are two important biotransformation processes of nitrogen cycling. In this study, we used soil (depths of 0-20, 25-45, and 55-75 cm) nitrification and denitrification rates as indicators to study the effects of revetment type on the spatial distribution of soil nitrogen cycling in tidal urban riparian zones adjacent to three revetments (permeable concrete pile revetments (PR), impervious masonry stone revetments (IR), and no revetments (NR)) at three distances (0.3, 0.6, and 1.0 m). Our results indicated that compared with natural riparian zones (NR), PR significantly improved soil nitrification and denitrification rates, while IR significantly improved soil nitrification rates but decreased denitrification rates (P < 0.05), which were totally different from the general perception, particularly in impervious revetments. Revetment type mainly affected the temporary inundation zones (0-20 cm). For example, in the temporary inundation zones, the variation in soil denitrification rates was 14.49 mg kg(-1) h(-1), while in the frequent inundation zones (25-45 cm) and the permanent inundation zones (55-75 cm), the variations were 3.26 and 2.94 mg kg(-1) h(-1), respectively. Soil compaction was probably the main constraint factor for soil nitrification in natural riparian zones, soil organic carbon (SOC) and nitrogen availability were probably the main constraint factors for soil denitrification adjacent to impervious revetments. In order to take full advantage of the structural characteristics of impervious revetments and permeable revetments, the combination of impervious revetments in permanent inundation zones and permeable revetments in temporary inundation zones could be optimally designed to enhance soil nitrogen cycling function of tidal urban riparian zones during revetment construction.
机译:河流渠道和河岸区之间的破坏是城市河岸区结构修改的重要因素,特别是在与它们相邻的区域中。虽然有很多关于潮汐城市河岸区的破坏稳定性的研究,但是破坏对它们附近的河岸区氮气循环的定量影响仍不清楚。潮汐河岸区比正常的河岸地区经历更频繁的河流 - 土壤交换,因此,修饰可能对氮循环产生更大的影响。硝化和反硝化是氮循环的两个重要的生物转化过程。在这项研究中,我们使用土壤(深度为0-20,25-45和55-75厘米)的硝化和反硝化率作为研究护套类型对潮汐城市河岸区土壤氮循环空间分布的指标毗邻三次修复(可渗透的混凝土桩修复(PR),不透水砌体石像(IR),三个距离(0.3,0.6和1.0米)没有修复(NR))。我们的结果表明,与自然河岸区(NR)相比,PR显着改善了土壤硝化和脱氮率,而IR显着提高土壤硝化率,但减少抵抗率(P <0.05),与普遍感知有关不透水的修道院。护垫型主要影响临时淹没区域(0-20厘米)。例如,在临时淹没区中,土壤脱氮率的变化为14.49mg kg(-1)h(-1),而在频繁的淹没区(25-45cm)和永久淹没区(55-75 cm),变化分别为3.26和2.94mg kg(-1)h(-1)。土壤压实可能是天然河岸地区土壤硝化的主要约束因素,土壤有机碳(SoC)和氮可用性可能是邻近不透水的破坏性的土壤反硝化的主要约束因素。为了充分利用不透水的破坏和可渗透的破坏的结构特征,可以最佳地设计永久性淹没区内的不透气破坏和渗透性修复的组合,以提高潮汐城市河岸区的土壤氮循环功能建造。

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