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[渠化对三江平原铁沉积的影响]

[Effects of Canalization on the Iron Deposition in Sanjiang Plain].

作者信息

Su Wen-hui, Yu Xiao-fei, Wang Guo-ping, Luan Jin-hua, Zou Yuan-chun

出版信息

Huan Jing Ke Xue. 2015 Apr;36(4):1431-6.

Abstract

Canalization is the representative process and landscape of wetland reclamation. A typical ditch system of four levels near the Honghe National Nature Reserve in Sanjiang Plain was selected. Deposition plates were set on the sediments along the ditch level and the remained natural wetland nearby was quantitatively sampled for two years as the control. The deposition fluxes, total iron concentration, iron oxides and their components, as well as biogenic elements in the sediments collected by deposition plates were measured. The results showed that the litter, mud/sand and total deposition fluxes showed no significant differences between different ditch levels, with the means of (57.00 ± 16.90) g x (m2 x a)(-1), (3 997.57 ± 798.98) g x (m2 x a)(-1) and (4054.57 ± 792.91) g x (m2 x a)(-1), respectively. The litter flux decreased with the increase of ditch level, and the flux in the natural wetland [ (120.26 ± 19.42) g x (m2 x a)(-1) ] was significantly greater than that of the ditches. The mud/sand [ (35.41 ± 11.15 ) g x (m2 x a)(-1)] and total deposition fluxes (155.67 ± 20.75) g x ( m2 x a ] were significantly smaller than those of the ditches. There were no significant differences in the total iron between different ditches and natural wetland, while the free iron oxide content in the ditch sediments was significantly lower than that of natural wetland sediment. Except for the main ditch, the amorphous and complex iron oxides in the other ditch and natural wetland sediments showed no significant differences. The free degree of the iron oxide in ditch sediments was 60.2% of that in the natural wetland, while the differences in the complex degree and the activated degree were insignificant. The differences in the total organic carbon, total nitrogen and total phosphorus were insignificant, and all were smaller than those of the natural wetland, with the percentages of 14.6%, 31.6% and 41.0%, respectively. It could be concluded that the effects of canalization on iron and biogenic elements were significant. Consequently, rational agricultural water managements are strongly recommended to avoid the potential environmental and ecological risks caused by canalization in Sanjiang Plain.

摘要

沟渠化是湿地开垦的典型过程和景观。选取了三江平原洪河国家级自然保护区附近一个典型的四级沟渠系统。沿沟渠层级在沉积物上设置沉积板,并对附近留存的天然湿地进行为期两年的定量采样作为对照。测定沉积板收集的沉积物中的沉积通量、总铁浓度、铁氧化物及其组分以及生源要素。结果表明,枯枝落叶、泥沙和总沉积通量在不同沟渠层级间无显著差异,均值分别为(57.00±16.90) g·(m²·a)⁻¹、(3997.57±798.98) g·(m²·a)⁻¹和(4054.57±792.91) g·(m²·a)⁻¹。枯枝落叶通量随沟渠层级增加而降低,天然湿地中的通量[(120.26±19.42) g·(m²·a)⁻¹]显著大于沟渠中的通量。泥沙通量[(35.41±11.15) g·(m²·a)⁻¹]和总沉积通量[(155.67±20.75) g·(m²·a)⁻¹]显著小于沟渠中的通量。不同沟渠和天然湿地之间的总铁无显著差异,但沟渠沉积物中的游离铁氧化物含量显著低于天然湿地沉积物。除主沟渠外,其他沟渠和天然湿地沉积物中的无定形铁氧化物和络合铁氧化物无显著差异。沟渠沉积物中铁氧化物的游离度为天然湿地的60.2%,而络合度和活化度差异不显著。总有机碳、总氮和总磷的差异不显著,且均小于天然湿地中的含量,分别为天然湿地的14.6%、31.6%和41.0%。可以得出结论,沟渠化对铁和生源要素的影响显著。因此,强烈建议进行合理的农业用水管理,以避免三江平原沟渠化带来的潜在环境和生态风险。

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