The indication of mire degeneration has appeared since 1960 s in the Zoige platean.
根据１９９６ ～１９９８ 年野外考察与研究获得的信息，结合前人研究的资料，论证了若尔盖高原沼泽区生态环境恶化、沼泽退化十分严重，其主要表现为：沼泽旱化，沼泽类型改变，沼泽逆向生态演替，沼泽区沙化，野生动物种类、种群数量减少，土壤质量下降，沼泽水质变劣，草场退化和鼠害猖獗。
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。
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。
A cutting in a peat bog.
泥炭沼泽地中的草地块
bogwood:Wood that has been preserved in a peat bog.
泥炭木,沼木:久埋于泥炭沼泽之中的树木。
Wood that has been preserved in a peat bog.
泥炭木，沼木久埋于泥炭沼泽之中的树木
A Study on the Transmission and Distribution of Rainfall in Hani-peat Mire
降水在哈泥泥炭沼泽中的传输与分配作用研究
FORMATION MECHANISM AND TIME-SPACE DISTRIBUTION OF COASTAL PEAT MOOR OF THE BOHAI BAY
渤海湾沿岸泥炭沼泽形成机制与时空分布
Study on the Distribution, Transformation and Environmental Effects of Nitrogen in Peat Mire;
泥炭沼泽氮素分布、转化及其环境效应研究
Study on Soil Water Physical Features of Typical Peat Swamps in Xiaoxing'anling Mountain
小兴安岭典型泥炭沼泽土壤水分物理性质研究
synsedimentary fallout ash alteration in the nearshore peat swamp and march environment.
它们是在近岸泥炭沼泽或沼泽环境中由同期降落的火山灰蚀变而成。
Studies on Population Ecology of Several Plants in the Northeast China's Oligotrophic Mires;
东北贫营养泥炭沼泽几种植物的种群生态学研究
ground pine thickly covered with bristly leaves; widely distributed in barren sandy or peaty moist coastal regions of eastern and southeastern United States.
长有毛状叶的石松；广泛分布于美国东部和东南部贫瘠的沙地或泥炭沼泽地区。
Records of Surface Wetness from Hani Mire in Changbai Mountains
哈泥泥炭藓泥炭记录的沼泽地表湿度变化
Any of certain other wetland areas, such as a fen, having a peat substrate.
沼泽地区任一种其它的湿地，有泥炭底面，如沼泽
Plant Diversity of Subalpine Sphagnum Mires in Western Hubei Province;
鄂西亚高山泥炭藓沼泽湿地的植物多样性
A swamp or bog formed by an accumulation of sphagnum moss, leaves, and decayed matter resembling peat.
厚苔沼类似泥炭地的沼泽地，由水藓、叶子和腐烂物质的堆积物形成
Soil water drainage and excessive grazing in pastureland of m ire and peat soils are accountable for the deterioration and quality decline of mire and peat soils.
人类疏干沼泽、过度放牧等活动是沼泽土和泥炭土退化、质量下降的主要原因。
Thick accumulations of peat can form only if the swamp basin slowly subsides.
只有当沼泽盆地慢慢下陷时，厚厚的泥炭堆积才能形成。
ON THE PURIFICATION EFFECTS OF THE SPHAGNUM WETLAND ON Cd(Ⅱ),Cu(Ⅱ),Pb(Ⅱ),Zn(Ⅱ) IN DAJIUHU BASIN OF SHENNONGJIA MOUNTAINS
神农架大九湖泥炭藓沼泽湿地对镉(Ⅱ)、铜(Ⅱ)、铅(Ⅱ)、锌(Ⅱ)的净化模拟
The Sphagnum Bog Plant Resources in Tianbaoyan Nature Reserve in Fujian
福建天宝岩自然保护区泥炭藓沼泽植物资源调查