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1.In Qinshui Basin, the fresh-water peat swamp facies and forest peat swamp facies were the sedimentary environments of forming good reservoirs, but the drained peat swamp fecies was difficult to form good reservoirs in general.
在沁水盆地，活水泥炭沼泽相以及森林泥炭沼泽相是形成有利储层的沉积环境，而干燥泥炭沼泽相一般难以形成有利的储层。收藏指正
2.Underground water table of Artificial Larch Swamp Forest declined 10-25cm and peat bed thinned out 0-25cm compared to natural.
人工落叶松沼泽林的地下水位较天然沼泽林下降了10-25cm,泥炭层厚度减少了0-25cm;收藏指正
3.Physical Mechanics Character Measurement of Peat Soil in Forest Area of Jilin
吉林林区泥炭质土物理力学性质测定收藏指正
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