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[长期施肥下黑土有机碳和全氮的分布与富集特征]

[Distribution and enrichment characteristics of organic carbon and total nitrogen in mollisols under long-term fertilization].

作者信息

Xu Xiang-ru, Luo Kun, Zhou Bao-ku, Wang Jing-kuan, Zhang Wen-ju, Xu Ming-gang

出版信息

Ying Yong Sheng Tai Xue Bao. 2015 Jul;26(7):1961-8.

PMID:26710620
Abstract

The characteristics and changes of soil organic carbon (SOC) and total nitrogen (TN) in different size particles of soil under different agricultural practices are the basis for better understanding soil carbon sequestration of mollisols. Based on a 31-year long-term field experiment located at the Heilongjiang Academy of Agricultural Sciences (Harbin) , soil samples under six treatments were separated by size-fractionation method to explore changes and distribution of SOC and TN in coarse sand, fine sand, silt and clay from the top layer (0-20 cm) and subsurface layer (20-40 cm). Results showed that long-term application of manure (M) increased the percentages of SOC and TN in coarse sand and clay size fractions. In the top layer, application of nitrogen, phosphorus and potassium fertilizers combined with manure (NPKM) increased the percentages of SOC and TN in coarse sand by 191.3% and 179.3% compared with the control (CK), whereas M application increased the percentages of SOC and TN in clay by 45% and 47% respectively. For subsurface layers, the increase rates of SOC and TN in corresponding parts were lower than that in top layer. In the surface and subsurface layers, the percentages of SOC storage in silt size fraction accounted for 42%-63% and 48%-54%, TN storage accounted for 34%-59% and 41%-47%, respectively. The enrichment factors of SOC and TN in coarse sand and clay fractions of surface layers increased significantly under the treatments with manure. The SOC and TN enrichment factors were highest in the NPKM, being 2.30 and 1.88, respectively, while that in the clay fraction changed little in the subsurface layer.

摘要

不同农业措施下土壤不同粒径颗粒中土壤有机碳(SOC)和全氮(TN)的特征及变化,是更好理解黑土土壤碳固存的基础。基于黑龙江省农业科学院(哈尔滨)开展的一项为期31年的长期田间试验,采用粒径分级法对六种处理下的土壤样品进行分离,以探究表层(0 - 20 cm)和亚表层(20 - 40 cm)粗砂、细砂、粉砂和黏土中SOC和TN的变化及分布。结果表明,长期施用有机肥(M)增加了粗砂和黏粒粒径组分中SOC和TN的占比。在表层,氮磷钾化肥与有机肥配施(NPKM)使粗砂中SOC和TN的占比相较于对照(CK)分别增加了191.3%和179.3%,而施用M使黏粒中SOC和TN的占比分别增加了45%和47%。对于亚表层,相应部分SOC和TN的增加速率低于表层。在表层和亚表层,粉砂粒径组分中SOC储量占比分别为42% - 63%和48% - 54%,TN储量占比分别为34% - 59%和41% - 47%。在有机肥处理下,表层粗砂和黏粒组分中SOC和TN的富集系数显著增加。SOC和TN富集系数在NPKM处理中最高,分别为2.30和1.88,而在亚表层黏粒组分中变化较小。

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