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荒漠生态条件下植物残体的分解特征和养分变化
孙本华1,2, 吕家珑2, 张一平2
1.中国科学院 阜康荒漠生态系统观测试验站;2.西北农林科技大学 资源环境学院
摘要:
以玉米秆为材料,研究了荒漠生态系统下残茬的腐解率和腐解物的有机C、N、K的含量、养分释放率及C/N的变化。结果表明,累积腐解率和有机C的分解率随时间的延长呈上升的趋势,0~46 d和46~92 d残茬腐解率分别为34.6%和11.9%,残茬有机C的分解率分别为34.9%和12.5%。腐解残留物的有机C、N和K的含量存在不同的变化规律,随时间的推移,有机C的含量先缓慢下降,184~350 d基本不变,然后又缓慢下降;氮含量则是先逐渐上升,138 d后基本不变;K含量在0~46 d迅速下降,然后趋于缓慢,184 d后基本不变。随腐解时间的延长,N和K的残留量逐渐减少,304 d后基本不变。N在0~46 d和46~92 d的释放率最大,分别达9.3%和9.0%;K的释放集中在0~46 d,释放率达80.4%,以后则变化不大,在90%左右。腐解残留物的C/N先迅速下降,138 d后基本不变,最终为26.3。
关键词:  荒漠生态  残茬分解  养分释放
DOI:
分类号:
基金项目:中国科学院阜康荒漠生态系统观测试验站开放基金资助项目(20020009)
The characteristics of decomposition and variation ofnutrient elements of plant residue in desert ecosystem
Abstract:
Quantitative studies on changes of decomposition rate,C/N ratio,N,K and organic C of corn residue during decomposition in desert ecosystem were carried out in Fukang,Xinjiang.Results showed that accumulative decay rate and organic C decomposition rate of corn residues increased when the decomposition time was increased.The decay rate in 0-46 d and 46-92 d was 34.6% and 11.9%,respectively.The organic C decomposition rate in 0-46 d and 46-92 d was 34.9% and 12.5%,respectively.The changes of organic C,N and K contents in decay remanent were different.Organic C contents decreased slowly first,then kept on at 184-350 d,then decreased slowly again.The nitrogen contents increased gradually first,then kept on after 138 d.The K contents decreased quickly from 6.53% to 1.92% at 0-46 d,then decreased slowly and kept on after 304 d.The releasing rates of N in 0-46 d and 46-92 d were great,and reached 9.3% and 9.0%,respectively.The releasing rate of K reached 80.4% in 46 d,then changed around 90%.The C/N ratio of decay remanent decreased quickly first,then didn’t change on the whole after 138 d,finally was 26.3.
Key words:  desert ecosystem  residue decomposition  nutrient releasing