跨地带土壤置换实验研究  被引量:1

The experimental study on trans-regional soil replacement

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作  者:靳英华[1] 许嘉巍[1] 秦丽杰[1] 

机构地区:[1]东北师范大学地理科学学院,长春130024

出  处:《生态学报》2014年第2期509-516,共8页Acta Ecologica Sinica

基  金:国家自然科学基金资助项目(41171072);中国地震局资助项目(201208005)

摘  要:以温带针阔混交林暗棕壤地带内的白浆土、草甸土、泥炭土为原料,以长白山自然保护区内的寒温带山地棕色针叶林土为置换对象,完成了仿自然原型的土壤合成,进行了跨地带的土壤置换与植被生长实验研究。结果表明:①山地棕色针叶林土的腐殖质层厚度、酸度和速效氮含量为植被生长的限制性因子;②合成土壤理化指标必须以原生土壤限制因子拐点(值)指标为确定依据,作为合成土壤的关键性指标;③在长白山采用泥炭土与草甸土各占1/4,白浆土占1/2进行混合,土层厚度40cm,并使用石灰进行调酸达到中性后,植被恢复效果最好、造价最低。When people did ecological restoration, it was very difficult to achieve the trans-regional soil replacement. Basalt platform is distributed around the Changbai Mountain Nature Reserve. The intrazonality soil ( i.e. baijiang soil, peat soil and meadow soil) in the temperate humid climate zone is developed widely on basalt platform, howerer, the zonality soil such as dark brown earth is rare. The mountain brown coniferous forest soil, baijiang soil, peat soil and meadow soil are not in the same physical geographic zone, and there are significant differences in their physical and chemical properties, thus, it is not easy to complete soil replacement directly. In this zone, we could use the synthesis soil which is artificially synthesized with baijiang soil, peat soil and meadow soil to instead of the mountain brown coniferous forest soil. In this study, the baijiang soil, peat soil and meadow soil in the dark brown soil zone in the temperate broadleaved-coniferous mixed forest were used as raw materials, and the mountain brown coniferous forest soil in cold temperate zone in Changbai Mountain Nature Reserve was used as replacement object. Firstly, we completed soil synthesis taking the imitates the natural prototype principle, and then, conducted the experimental research on trans-regional soil replacement and plant growth. The results showed that the differences of soils were significant in the distribution of the content of every soil grain size group ( %), humus layer thickness (10--20 cm), pH (5.9--7.5), and the available nitrogen (N) content (57.8--100.7 g/kg) in the mountain brown coniferous forest soil zone. The limited factors of plant growth were humus layer thickness, pH, and available N content of mountain brown coniferous forest soil. Plant growth condition was better as the humus layer thickness was 40cm, pH was 7.0 and available N content was 80 mg/kg which were the inflection point value of the mountain brown coniferous forest soil limited factors. Therefore, the inflection po

关 键 词:山地棕色森林土 地带 土壤置换 

分 类 号:S15-3[农业科学—土壤学]

 

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