摘要
研究了黄土高原南部地区不同土壤类型及不同利用方式下土壤微生物摄碳、氮和可溶性有机碳、氮的含量。结果表明:不同土地利用方式下,土壤微生物量碳、氮和可溶性有机碳、氮含量均为林地〉农田,其中林地枯枝落叶层〉林地O~20cm土层。农田土壤微生物量碳、氮的含量均为红油土〉黑垆土〉淋溶褐土;农田土壤中可溶性有机碳含量为淋溶褐土〉红油土〉黑垆土,而可溶性有机氮含量则为黑垆土〉红油土〉淋溶褐土。方差分析表明,不同土壤类型土壤微生物量氮含量之间的差异达显著水平,而不同土壤类型间土壤微生物量碳、可溶性有机碳、氯含量之间的差异未达显著水平。土壤微生物量碳、氮占土壤有机碳和全氮的比例明显高于可溶性有机碳、氮占土壤有机碳和全氮的比例。相关分析发现,土壤微生物量碳与可溶性有机碳之间以及土壤微生物量氮与可溶性有机氮之间的相关性达显著或极显著水平,说明土壤微生物量碳、氮和土壤可溶性有机碳、氮之间有密切联系。
This study was conducted to determine the contents of soil microbial biomass carbon (BC), and nitrogen (BN), K2SO4-extractable organic carbon (DOC), and nitrogen (SON) in three different soil types and under two different use patterns in the south part of Loess Plateau. The results showed that the contents of BC, BN, DOC and SON in the forest soils were higher than those in the arable soils; and the concentrations of thcse parameters in the forest litter were significantly higher than those in the 0-20 cm soil layers. Under the different agricultural cultivation, the concentrations of BC and BN in the anthrosols were higher than those in thc isohumisols and the argosols. The concentration of DOC in the argosols was higher than that in the anthrosols and the isohu- misols. The concentration of SON in the isohumisols was higher than that in the anthrosols and the argosols. Soil types had significant effect on the concentration of BN, but had no significant effect on the concentrations of BC, DOC and SON. The ratios of BC to soil organic C (BC/TC), and BN to soil total N (BN/TN) were significantlyhigher than the ratios of DOC to TC (DOC/TC), and SON to TN (SON/TN). There were significant positive correlations between BC, BN and DOC, SON, indicating the close relationships between BC, BN and DOC, SON.
出处
《水土保持学报》
CSCD
北大核心
2006年第6期103-106,132,共5页
Journal of Soil and Water Conservation
基金
国家自然科学基金项目(40571087
30370288和30230230)
黄土高原土壤侵蚀与旱地农业国家重点实验室基金(10501-160)
关键词
黄土高原
土壤类型
土壤微生物量碳、氮
可溶性有机碳、氮
Loess Plateau
soil types
microbial biomass carbon (BC), nitrogen (BN)
K2SO4-extractableorganic carbon (DOC), nitrogen (SON)