河南理工大学学报:自然科学版
河南理工大學學報:自然科學版
하남리공대학학보:자연과학판
JOURNAL OF HENAN POLYTECHNIC UNIVERSITY
2012年
3期
352-356
,共5页
朱宁%赵同谦%肖春艳%焦立恒%张坤峰
硃寧%趙同謙%肖春豔%焦立恆%張坤峰
주저%조동겸%초춘염%초립항%장곤봉
滨河湿地%土壤微生物%放线茵
濱河濕地%土壤微生物%放線茵
빈하습지%토양미생물%방선인
riparian wetland%soil microorganism%distribution characters
对河滩退耕地恢复为湿地植被后典型湿地植被群落不同沉积层的土壤微生物变化特征进行了初步研究.结果表明,河滩退耕地恢复前后,土壤中的微生物主要集中在0~10em的表土层,其数量以细菌占绝对优势(占微生物总数的62.87%~96.64%);随深度的增加,细菌数量呈递减趋势,放线菌数量呈递增趋势,真菌数量则变化不明显.同时,退耕恢复后,3类微生物数量呈增加趋势,说明经过一个恢复周期后,植物群落恢复对土壤微生物的数量产生了显著影响.细菌数量与全氮和有机质呈显著相关(P〈0.05),说明土壤主要养分在一定程度上影响了细菌分布.
對河灘退耕地恢複為濕地植被後典型濕地植被群落不同沉積層的土壤微生物變化特徵進行瞭初步研究.結果錶明,河灘退耕地恢複前後,土壤中的微生物主要集中在0~10em的錶土層,其數量以細菌佔絕對優勢(佔微生物總數的62.87%~96.64%);隨深度的增加,細菌數量呈遞減趨勢,放線菌數量呈遞增趨勢,真菌數量則變化不明顯.同時,退耕恢複後,3類微生物數量呈增加趨勢,說明經過一箇恢複週期後,植物群落恢複對土壤微生物的數量產生瞭顯著影響.細菌數量與全氮和有機質呈顯著相關(P〈0.05),說明土壤主要養分在一定程度上影響瞭細菌分佈.
대하탄퇴경지회복위습지식피후전형습지식피군락불동침적층적토양미생물변화특정진행료초보연구.결과표명,하탄퇴경지회복전후,토양중적미생물주요집중재0~10em적표토층,기수량이세균점절대우세(점미생물총수적62.87%~96.64%);수심도적증가,세균수량정체감추세,방선균수량정체증추세,진균수량칙변화불명현.동시,퇴경회복후,3류미생물수량정증가추세,설명경과일개회복주기후,식물군락회복대토양미생물적수양산생료현저영향.세균수량여전담화유궤질정현저상관(P〈0.05),설명토양주요양분재일정정도상영향료세균분포.
This paper generally describes the distribution characteristics of soil microbial population in different soil layers of different wetland vegetation communities after artificial restoration. The results show that the bacteria takes up the biggest share in .total soil microorganism, and the proportion reaches 62.87% - 96.64% . Most of soil microorganism are present in the upper 0 - 10 cm layer. The bacteria quantity decreases and the actinomycetes quantity increases with soil depth increasing, but the variation of fungus is not significant. The total amounts of three kinds microbes increase after wetland restoration, which show that wetland vegetation restoration has made a significant influence on microbial population after a growth cycle. The bacteria quantity has significant correlation with soil TN and OM (p 〈0.05 ) , which show that the soil nutrient affects the distribution of bacteria in some degree.