湖北农业科学
湖北農業科學
호북농업과학
Hubei Agricultural Sciences
2015年
17期
4168-4172
,共5页
张耿杰%白中科%张川%张建生
張耿傑%白中科%張川%張建生
장경걸%백중과%장천%장건생
复垦%表层土壤%理化性质%平朔矿区
複墾%錶層土壤%理化性質%平朔礦區
복은%표층토양%이화성질%평삭광구
reclamation%surface soil%physic-chemical properties%Pingshuo mining area
通过对平朔矿区原地貌、未复垦及不同复垦模式下典型样地表层土壤在0~10 cm和10~20 cm处的容重、田间持水量、有机质、全氮和碳氮比的特征进行横向、纵向与综合分析,揭示复垦土地表层土壤理化性质的变化规律。结果表明,未复垦样地除了容重以外的其他理化指标均值都低于原地貌样地和复垦样地;复垦样地中土石混排的林地表层土壤中有机质含量最高。各样地容重在0~10 cm均值都低于10~20 cm土层;仅未复垦样地的田间持水量均值在0~10 cm低于10~20 cm土层;有机质、全氮和碳氮比在0~10 cm的均值一般高于10~20 cm土层。原地貌样地中容重与田间持水量和有机质呈显著负相关;未复垦样地中容重与土壤化学指标呈极显著正相关,而田间持水量与其他指标呈极显著负相关;复垦样地中指标的相关性类似原地貌样地,只是容重与全氮之间呈显著负相关。建议土石混排方式下的复垦方向为林地,以纯土壤为复垦物质条件下的最初复垦方式为草地,在复垦10年后可考虑改变土地利用方式为耕地。
通過對平朔礦區原地貌、未複墾及不同複墾模式下典型樣地錶層土壤在0~10 cm和10~20 cm處的容重、田間持水量、有機質、全氮和碳氮比的特徵進行橫嚮、縱嚮與綜閤分析,揭示複墾土地錶層土壤理化性質的變化規律。結果錶明,未複墾樣地除瞭容重以外的其他理化指標均值都低于原地貌樣地和複墾樣地;複墾樣地中土石混排的林地錶層土壤中有機質含量最高。各樣地容重在0~10 cm均值都低于10~20 cm土層;僅未複墾樣地的田間持水量均值在0~10 cm低于10~20 cm土層;有機質、全氮和碳氮比在0~10 cm的均值一般高于10~20 cm土層。原地貌樣地中容重與田間持水量和有機質呈顯著負相關;未複墾樣地中容重與土壤化學指標呈極顯著正相關,而田間持水量與其他指標呈極顯著負相關;複墾樣地中指標的相關性類似原地貌樣地,隻是容重與全氮之間呈顯著負相關。建議土石混排方式下的複墾方嚮為林地,以純土壤為複墾物質條件下的最初複墾方式為草地,在複墾10年後可攷慮改變土地利用方式為耕地。
통과대평삭광구원지모、미복은급불동복은모식하전형양지표층토양재0~10 cm화10~20 cm처적용중、전간지수량、유궤질、전담화탄담비적특정진행횡향、종향여종합분석,게시복은토지표층토양이화성질적변화규률。결과표명,미복은양지제료용중이외적기타이화지표균치도저우원지모양지화복은양지;복은양지중토석혼배적임지표층토양중유궤질함량최고。각양지용중재0~10 cm균치도저우10~20 cm토층;부미복은양지적전간지수량균치재0~10 cm저우10~20 cm토층;유궤질、전담화탄담비재0~10 cm적균치일반고우10~20 cm토층。원지모양지중용중여전간지수량화유궤질정현저부상관;미복은양지중용중여토양화학지표정겁현저정상관,이전간지수량여기타지표정겁현저부상관;복은양지중지표적상관성유사원지모양지,지시용중여전담지간정현저부상관。건의토석혼배방식하적복은방향위임지,이순토양위복은물질조건하적최초복은방식위초지,재복은10년후가고필개변토지이용방식위경지。
To assess the impacts of reclamation on topsoil physic-chemical properties in Pingshuo mining area, this study compared bulk density(BD), field capacity(FC), organic matter(OM),total nitrogen(TN) and C/N between 0~10 cm and 10~20 cm of topsoil in typical plots through the transverse,longitudinal and comprehensive analysis.The results showed that all the physic-chemical indicators except BD of unreclaimed plots were lower than those of original plots and reclaimed plots. The plot with woodland heaped by earth-rock had the highest OM among all plots. BD of all plots in 0~10 cm was lower than in 10~20 cm,while unreclaimed plots had lower FC in 0~10 cm than in 10~20 cm. Most plots had higher OM,TN and C/N at 0~10 cm than at 10~20 cm layer. BD was significantly negatively correlated with FC and OM in original plots. BD and soil chemical indicators showed a significant positive correlation in unreclaimed plots,while the FC was significantly negatively correlated with other indicators. Relativity of indicators in reclaimed plots were similar as original plots,just the relativity of BD and TN was significantly negative. The reclamation direction of woodland was suggested in lands with the woodland heaped by earth-rock,while other lands were rescaled to grassland.