1) sphagnum wetland
泥炭藓沼泽湿地
1.
In the July of the year 2008,the purification effects of the sphagnum wetland in Dajiuhu basin of Shennongjia mountains on metal ions Cd(Ⅱ),Cu(Ⅱ),Pb(Ⅱ),Zn(Ⅱ) were studied using simulated wetland on the basis of the research in August,2007.
在2007年8月研究的基础上,于2008年7月在神农架大九湖泥炭藓沼泽湿地采用自制简易模拟装置进行现场模拟实验,深入研究了泥炭藓沼泽湿地对不同浓度的金属污染物镉(Ⅱ)、铜(Ⅱ)、铅(Ⅱ)、锌(Ⅱ)的净化作用。
2) Sphagnum mire
泥炭藓沼泽
1.
Sphagnum mire occupy extensive tracts of land throughout the Boreal and Subarctic regions.
泥炭藓沼泽多分布于北半球的温带到负极带地区,在我国,泥炭藓沼泽主要发育在大、小兴安岭和长白山等地。
3) peat mire
泥炭沼泽湿地
1.
Carbon dioxide flux from peat mire in Ruoergai plateau;
若尔盖高原泥炭沼泽湿地CO_2呼吸通量特征
4) peat and mire
泥炭和沼泽地
5) peat swamp
泥炭沼泽
1.
On the basis of study on the petrographic characteristics of coal 2 -2 in Shenmu Coalfield,three types of peat swamp are recognized,i.
在研究神木煤田2-2煤层煤岩特征的基础上,划分了三种泥炭沼泽类型,即开阔水体草本沼泽、陆地森林沼泽和潮湿森林沼泽。
2.
Soil water physical features of five kinds of typical peat swamps were compared in Xiaoxing\'anling Mountain,and the following results were obtained.
对小兴安岭5类典型泥炭沼泽土壤水分物理性质进行对比研究,结果表明:落叶松-杜香-泥炭藓沼泽土壤容重最小,非毛管孔隙最高,持水性最好;漂筏苔草沼泽和油桦-笃斯越桔-修氏苔草沼泽次之,修氏苔草沼泽和白桦-油桦-小叶章沼泽相对较差。
补充资料:泥炭藓沼泽中近于死亡的“小老树”
郎惠卿提供
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