黑土有机碳、氮及其活性对长期施肥的响应 |
摘要点击 4675 全文点击 1926 投稿时间:2012-04-17 修订日期:2012-07-31 |
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中文关键词 长期施肥 有机碳 全氮 矿质氮 土壤微生物生物量碳氮 可溶性碳氮 |
英文关键词 long-term fertilization soil organic carbon total nitrogen mineral nitrogen soil microbial biomass carbon and nitrogen dissolved organic carbon and nitrogen |
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中文摘要 |
以长期定位试验为基础,研究不同长期施肥模式对中国东北黑土表层(0~20 cm)及亚表层(20~40 cm)土壤碳、氮的影响.结果表明,有机肥的施入显著提高了表层土壤有机碳(SOC)和全氮(TN)含量,其中以有机无机配施处理最为显著.与不施肥相比,常量和高量有机无机配施分别增加了表层SOC含量24.6%和25.1%,分别增加了表层土壤TN含量29.5%和32.8%,亚表层土壤SOC和TN含量对施肥无响应.尽管常量及高量有机无机配施分别增加了黑土0~40 cm土壤碳储量11.6%和7.6%、氮储量17.3%和12.7%,但各处理之间无显著差异,仅增加了黑土碳、氮储量的变异性.与不施肥相比,有机肥的施用不仅显著增加了表层和亚表层土壤微生物生物量碳、氮(SMBC、SMBN)及可溶性碳、氮(DOC、DN)的含量,且显著提高了这些组分在总有机碳、全氮中所占的比例.有机无机配施处理能使表层土壤SMBC/SOC、SMBN/TN值分别提高0.36~0.59和1.21~1.95个百分点,而DOC/SOC、DN/TN也分别达到0.53%~0.72%和1.41%~1.78%.土壤微生物生物量碳氮、可溶性碳氮及其在总有机碳、氮中所占的比例对于施肥的响应在土壤剖面上表现更为敏感,更能反映土壤肥力对于长期施肥的响应.有机肥的施入尤其是有机无机配施能显著提高黑土表层和亚表层土壤有机碳、氮活性,有利于提升土壤肥力和养分供应能力,但同时也导致了农田系统碳、氮的大量损失,容易引起潜在的环境污染. |
英文摘要 |
Based on the long-term fertilization experiments, effects of various fertilization practices on the soil organic carbon (SOC) and total nitrogen (TN) in the surface (0-20 cm) and subsurface (20-40 cm) black soil in northeast China were studied. Results showed that, compared with the CK, long-term application of organic manure, especially the combination of mineral fertilizers and organic manure significantly increased the organic SOC and TN in the surface soil. Application of mineral fertilizers plus organic manure with conventional (NPM) and high application (N2P2M2) rate increased SOC significantly by 24.6% and 25.1%, and TN by 29.5% and 32.8%, respectively. However, there was no significant difference among the treatments for SOC and TN at the subsurface. Compared with the CK (CKh), mineral fertilizer plus organic manure (NPM and N2P2M2) did not only increase the soil microbial biomass carbon (SMBC) and nitrogen (SMBN), dissolved organic carbon (DOC) and nitrogen (DN), but also significantly increased the ratio of SMBC and DOC to SOC, SMBN and TN to TN. Application of the NPM and N2P2M2 increased the value of SMBC/SOC by 0.36 to 0.59 and SMBN/TN by 1.21 to 1.95 percentage points, respectively. The value of DOC/SOC and DN/TN ranged from 0.53% to 0.72% and 1.41% to 1.78%, respectively. This result indicated that SMBC, SMBN, DOC, DN and SMBC/SOC, SMBN/TN, DOC/SOC, DN/TN were more sensitive than SOC and TN to long-term fertilization in the soil profile, and were better indicators for the impact of long-term fertilization soil fertility. The concluded that the application of manure especially manure plus mineral fertilizers can increase soil nutrients activity in the surface and subsurface black soil, acting as a helpful practice to improve soil fertility and the ability of nutrient supply, while it may cause potential environment pollution on carbon and nitrogen loss in the agroecosystem. |
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