College of Environmental Science and Engineering, Hunan University, Changsha, PR China ; Key Laboratory of Environmental Biology and Pollution Control (Hunan University), Ministry of Education, Changsha, PR China.
PLoS One. 2013 Oct 17;8(10):e77838. doi: 10.1371/journal.pone.0077838. eCollection 2013.
The effects of water erosion (including long-term historical erosion and single erosion event) on soil properties and productivity in different farming systems were investigated. A typical sloping cropland with homogeneous soil properties was designed in 2009 and then protected from other external disturbances except natural water erosion. In 2012, this cropland was divided in three equally sized blocks. Three treatments were performed on these blocks with different simulated rainfall intensities and farming methods: (1) high rainfall intensity (1.5-1.7 mm min(-1)), no-tillage operation; (2) low rainfall intensity (0.5-0.7 mm min(-1)), no-tillage operation; and (3) low rainfall intensity, tillage operation. All of the blocks were divided in five equally sized subplots along the slope to characterize the three-year effects of historical erosion quantitatively. Redundancy analysis showed that the effects of long-term historical erosion significantly caused most of the variations in soil productivity in no-tillage and low rainfall erosion intensity systems. The intensities of the simulated rainfall did not exhibit significant effects on soil productivity in no-tillage systems. By contrast, different farming operations induced a statistical difference in soil productivity at the same single erosion intensity. Soil organic carbon (SOC) was the major limiting variable that influenced soil productivity. Most explanations of long-term historical erosion for the variation in soil productivity arose from its sharing with SOC. SOC, total nitrogen, and total phosphorus were found as the regressors of soil productivity because of tillage operation. In general, this study provided strong evidence that single erosion event could also impose significant constraints on soil productivity by integrating with tillage operation, although single erosion is not the dominant effect relative to the long-term historical erosion. Our study demonstrated that an effective management of organic carbon pool should be the preferred option to maintain soil productivity in subtropical red soil hilly region.
本研究调查了不同农业系统中水力侵蚀(包括长期历史侵蚀和单次侵蚀事件)对土壤性质和生产力的影响。2009 年,设计了一个具有均匀土壤性质的典型坡耕地,并使其免受除自然水力侵蚀以外的其他外部干扰。2012 年,将该耕地分为三个面积相等的区块。在这些区块上进行了三种不同的模拟降雨强度和耕作方式的处理:(1)高降雨强度(1.5-1.7mm min(-1)),免耕作业;(2)低降雨强度(0.5-0.7mm min(-1)),免耕作业;和(3)低降雨强度,耕作作业。所有区块均沿坡向分为五个面积相等的小区,以定量描述三年历史侵蚀的影响。冗余分析表明,长期历史侵蚀的影响显著导致免耕和低降雨侵蚀强度系统中土壤生产力的大部分变化。模拟降雨强度对免耕系统中的土壤生产力没有显著影响。相比之下,在相同的单次侵蚀强度下,不同的耕作操作会导致土壤生产力的统计差异。土壤有机碳(SOC)是影响土壤生产力的主要限制变量。长期历史侵蚀对土壤生产力变化的大部分解释源于其与 SOC 的共同作用。SOC、全氮和全磷由于耕作作业被发现是土壤生产力的回归变量。总的来说,本研究提供了强有力的证据表明,单次侵蚀事件也可以通过与耕作作业相结合对土壤生产力施加显著限制,尽管单次侵蚀相对于长期历史侵蚀并不是主要影响因素。我们的研究表明,在亚热带红壤丘陵区,有效管理有机碳库应该是维持土壤生产力的首选方案。