We selected adjacent Deyeuxia angustifolia meadow and farmland cultivated 1,3,5,9,15,25 and 35 years, to study cultivation effects on soil biological properties and organic matter dynamics in the Sanjiang Plain in Northeast China.The results showed that cultivation resulted in decrease in the microbial biomass carbon (MBC), microbial quotient(MQ), and basal respiration (BR).While, metabolized quotient (qCO2), potential respiration/basal respiration(PR/BR), and PR/MBC ratios obviously increased with cultivation.Converting wetland soil into agriculture soil resulted in significant decline in carbon availability and efficiency of microbial populations in conserving C.There are clear relationships between soil microbial properties.The method evaluating more parameters simultaneously can provide complete and true information about the soil microorganisms and carbon dynamics.
ZHANG Jin-Bo, SONG Chang-Chun, YANG Wen-Yan
. Cultivation Effects on Soil Organic Carbon Dynamics in Sanjiang Plain, Northeast China[J]. SCIENTIA GEOGRAPHICA SINICA, 2006
, 26(3)
: 340
-344
.
DOI: 10.13249/j.cnki.sgs.2006.03.340
[1] Martens R.Current methods for measuring microbial biomass C in soil:Potentials and limitations[J].Biology Fertilizer Soils,1995,19:87~99.
[2] 刘兴土.松嫩-三江平原湿地资源及其可持续利用[J].地理科学,1997,17(增刊):451~460.
[3] 汪爱华,张树清,何艳芬.RS和GIS支持下的三江平原沼泽湿地动态变化研究[J].地理科学,2002,22 (5):636~640.
[4] 李 颖,张养贞,张树文.三江平原沼泽湿地景观格局变化及其生态效应[J].地理科学,2002,22 (6):677~689.
[5] 刘兴土,马学慧.三江平原自然环境变化与生态保育[M].北京:科学出版社,2002.
[6] 闫敏华,邓 伟,陈泮勤.三江平原气候突变分析[J].地理科学,2003,23(6):661~668.
[7] 刘景双,杨继松,于君宝,等.三江平原沼泽湿地土壤有机碳的垂直分布特征研究[J].水土保持学报,2003,17 (3):5~8.
[8] 张金波,宋长春,杨文燕.三江平原不同土地利用方式碳、氮动态变化[J].吉林农业大学学报,2003,25 (5):548~550.
[9] 宋长春,王毅勇,闫百兴,等.沼泽湿地开垦后土壤水热条件变化与碳、氮动态[J].环境科学,2004,25 (3):168~172.
[10] 胡金明,刘兴土.三江平原土壤质量变化评价与分析[J].地理科学,1999,19(5):417~421.
[11] 鲁如坤(主编).土壤农业化学分析法[M].北京:中国农业科技出版社,2000.231~233.
[12] Hofman J,Bezchlebová J,Duek L,et al.Novel approach to monitoring of the soil biological quality[J].Environment International,2003,28 (8):771-778.
[13] Insam H and Domsch K H.Relationship between soil organic carbon and microbial biomass on chronosequences of reclamation sites[J].Microbial Ecology,1988,15:177-188.
[14] Cheng W X,Zhang Q L,Coleman D C,et al.Is available carbon limiting microbial respiration in the rhizosphere? [J].Soil Biol.Biochem,1996,28 (10-11):1283-1288.
[15] Powlson D S,Brookes P C,Christensen B T.Measurement of soil microbial biomass provides an early indication of changes in total soil organic matter due to straw incorporation[J].Soil Biol.Biochem,1987,19 (2):159-164.
[16] Saggar S,Yeates G W,Shepherd T G.Cultivation effects on soil biological properties,microfauna and organic matter dynamics in Eutric Gleysol and Gleyic Luvisol soils in New Zealand[J].Soil & Tillage Research,2001,58 (1-2):55-68.