Zhang Wen-Juan, Liao Hong-Kai, Long Jian, Li Juan, Liu Ling-Fei
Huan Jing Ke Xue. 2015 Mar;36(3):1053-9.
Taking 5-year-old Chinese prickly ash orchard (PO-5), 17-year-old Chinese prickly ash orchard (PO- 17), 30-year-old Chinese prickly ash orchard (PO-30) and the forest land (FL, about 60 years) in typical demonstration area of desertification control test in southwestern Guizhou as our research objects, the aim of this study using a batch incubation experiment was to research the mineralization characteristics of soil organic carbon and changes of the labile soil organic carbon contents at different depths (0-15 cm, 15-30 cm, and 30-50 cm). The results showed that: the cumulative mineralization amounts of soil organic carbon were in the order of 30-year-old Chinese prickly ash orchard, the forest land, 5-year-old Chinese prickly ash orchard and 17-year-old Chinese prickly ash orchard at corresponding depth. Distribution ratios of CO2-C cumulative mineralization amount to SOC contents were higher in Chinese prickly ash orchards than in forest land at each depth. Cultivation of Chinese prickly ash in long-term enhanced the mineralization of soil organic carbon, and decreased the stability of soil organic carbon. Readily oxidized carbon and particulate organic carbon in forest land soils were significantly more than those in Chinese prickly ash orchards at each depth (P < 0.05). With the increasing times of cultivation of Chinese prickly ash, the contents of readily oxidized carbon and particulate organic carbon first increased and then declined at 0-15 cm and 15-30 cm depth, respectively, but an opposite trend was found at 30-50 cm depth. At 0-15 cm and 15-30 cm, cultivation of Chinese prickly ash could be good for improving the contents of labile soil organic carbon in short term, but it was not conducive in long-term. In this study, we found that cultivation of Chinese prickly ash was beneficial for the accumulation of labile organic carbon at the 30-50 cm depth.
以贵州省西南部荒漠化防治试验典型示范区内5年生花椒园(PO - 5)、17年生花椒园(PO - 17)、30年生花椒园(PO - 30)以及林地(FL,约60年)为研究对象,本研究采用批次培养试验,旨在研究不同深度(0 - 15厘米、15 - 30厘米和30 - 50厘米)土壤有机碳的矿化特征以及土壤活性有机碳含量的变化。结果表明:在相应深度,土壤有机碳的累积矿化量顺序为30年生花椒园、林地、5年生花椒园和17年生花椒园。各深度花椒园CO₂ - C累积矿化量占SOC含量的分配比例均高于林地。长期种植花椒增强了土壤有机碳的矿化作用,降低了土壤有机碳的稳定性。各深度林地土壤中的易氧化有机碳和颗粒有机碳显著多于花椒园(P < 0.05)。随着花椒种植年限增加,0 - 15厘米和15 - 30厘米深度的易氧化有机碳和颗粒有机碳含量分别先增加后下降,但30 - 50厘米深度呈现相反趋势。在0 - 15厘米和15 - 30厘米深度,短期种植花椒有利于提高土壤活性有机碳含量,但长期来看则不利。本研究发现,花椒种植有利于30 - 50厘米深度活性有机碳的积累。