首页|旱区农牧交错带不同土地利用类型土壤碳氮磷及其生态化学计量特征

旱区农牧交错带不同土地利用类型土壤碳氮磷及其生态化学计量特征

扫码查看
为了阐明旱区农牧交错带土壤碳氮磷及其生态化学计量特征,选择了宁夏盐池县草地、灌丛沙堆、农田、林地、弃耕地、固定沙丘及流动沙丘为研究对象,采用了野外分层采样与室内实验方法,分析了浅层土壤的有机碳(SOC)、全氮(TN)、全磷(TP)含量及土壤 C、N、P 生态化学计量特征.结果表明:(1)研究区内SOC、TN 和 TP 的平均含量 2.623 g·kg-1、0.134 g·kg-1、1.239 g·kg-1,均表现为弃耕地>灌丛沙堆>农田>草地>林地>固定沙丘>流动沙丘.土壤C/N变异系数为 48.95%,土壤C/P,N/P变异系数分别为 110.54%、115.47%.(2)研究区内林地、灌丛、草地和农田的土壤养分显著高于固定和流动沙丘,且林地和灌丛沙堆土壤SOC和TN含量随土层深度增加呈递减趋势.N/P有显著差异,土壤 C/N 和 C/P 差异不显著.不同土地利用类型对土壤 C、N、P 含量和生态化学计量特征存在显著的影响,对土壤养分以及化学计量的垂直分布也影响显著.本研究可为旱区农牧交错带沙漠化治理及农田风蚀防治提供重要的理论依据.
Soil C,N,P and its ecological stoichiometry in farming-pastoral zone in arid region
In order to clarify the soil C,N,P and its ecological stoichiometric characteristics in the agro-pastoral ecotone in arid regions,grassland,shrub sand pile,farmland,forest land,abandoned farmland,fixed dune and mobile dune were selected as research objects.The contents of organic carbon(SOC),total nitrogen(TN)and total phosphorus(TP)and the ecological stoichiometry characteristics of C,N and P in shallow soil were analyzed.The results showed as follows.(1)The average contents of SOC,TN and TP in the study area were 2.623g·kg-1,0.134g·kg-1,1.239g·kg-1,which were characterized by abandoned farmland>shrub coppice dune>farmland>grassland>forest land>fixed dune>mobile dune.The coefficient of variation of soil C/N was 48.95%,and the coefficient of variation of soil C/P and N/P were 110.54%and 115.47%,respectively.(2)In the study area,soil nutrients in forest land,shrub coppice dune,grassland and farmland were significantly higher than those in fixed and mobile dunes,and SOC and TN contents in forest land and shrub coppice dunee showed a decreasing trend with the increase of soil depth.There was no significant difference between soil C/N and C/P,but significant difference between soil N/P.(3)SOC and TN were positively correlated with C/P and N/P,while soil P was not significantly correlated with C/N,C/P and N/P.Different land use types had significant effects on soil C,N,P contents and ecological stoichiometry,as well as on the vertical distribution of soil nutrients and stoichiometry.SOC content was closely related to TN content,and soil ecological stoichiometry was mainly affected by SOC and TN.The results can provide important theoretical basis for desertification combating and farmland wind erosion control in agro-pastoral ecotone in arid regions.

soil C,N,Pecological stoichiometryfarming-pastoral zone in arid region

展秀丽、董智今、马亚莉、靳聪伟

展开 >

宁夏大学地理科学与规划学院,银川 750021

西北农林科技大学水土保持研究所,杨凌 712100

土壤碳、氮、磷 生态化学计量 旱区农牧交错带

2024

生态科学
广东省生态学会 暨南大学

生态科学

CSTPCD北大核心
影响因子:0.464
ISSN:1008-8873
年,卷(期):2024.43(6)