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汉语拼音：zhǎo zé huà

存在泥炭化的土地长期过湿，在湿生作物作用或厌氧条件下进行的有机质的生物积累和矿质元素还原的过程。沼泽化土壤有机质多，植物养料的灰分元素缺乏，水分长期饱和，通气不良。排水可防止沼泽化的发生发展。

• Generally, soil nutrition content showed the pattern like this: K. tibetica swamp meadowSalix oritrepha shrub meadowK. pygmaca meadow.

  总体来看，土壤养分含量藏嵩草沼泽化草甸〉山生柳灌丛草甸〉小嵩草草甸。

• Study on Prevention and Control of Out-of-Dam swampiness in DingZhuang Reservoir

  丁庄水库防治坝外沼泽化研究

• Subgrade Stabilization and Ground Temperature Monitoring in Marshy FrozenSoil Sloped Wet Land

  冻土沼泽化斜坡湿地路基稳定与地温监测

• Evolution of community structure of aquatic macrophytes in East Taihu Lake and its wetlands

  东太湖水生植物群落结构的演变及其沼泽化

• Effect of Returning the Crop Stack into Subsoil on Improving The Marsh Bog Soil and Drainage

  秸秆心土还田改良沼泽化土壤排涝效果的研究

• Discussion on the marsh formation of burned area in forest

  森林火烧迹地土壤沼泽化问题的探讨

• Investigation on Community Structure and Biomass of Kobresia Tibetica Swamp Meadow in Dawutan

  大武滩藏嵩草沼泽化草甸群落结构及植物量调查研究

• Distribution of Water-soluble Ionic Iron of Deyeuxia angustifolia Marsh and Carex lasiocarpa Marsh in the Sanjiang Plain

  三江平原毛苔草沼泽和小叶章沼泽化草甸湿地水体中可溶性铁的分布特征