Ho Jun Jang, Mercedes Roman Dobarco, Budiman Minasny, Jose Padarian Campusano, Alex McBratney
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引用次数: 1
Abstract
The impact from humans on soils, particularly in terms of intensive agriculture, has been most noticeable in the last 200 years. Intensive agricultural activities have caused soil organic carbon (SOC) to decline in many parts of the world. However, there is a dearth of approaches that can spatially estimate the change of SOC due to human influence. Here, we used the concept of Pedogenon to stratify the landscape into soil classes called Pedogenons. Within each Pedogenon, we sampled representative soils under native vegetation and soils under intensive human management. We surveyed the lower Namoi Valley area, NSW, Australia (1700 km2), comprising 13 Pedogenons (soil classes) and analysed SOC on 99 soil cores. Using Digital Soil Mapping techniques, the SOC data were used for mapping SOC every 10 cm down to 1 m using environmental covariates. Sampling points under native vegetation were used to map SOC under the native state, and all data were used for mapping SOC current state. By comparing the SOC maps at two states (native and current), we assessed SOC change. The results show that the SOC loss in irrigated cropping areas was the largest, with surface SOC content decreased by 38%, followed by non-irrigated cropping (30% loss), and pasture (19% loss). All cropping areas show a decrease in SOC stock content at least 5 t C ha−1. SOC loss was greatest in the surface soils and decreased exponentially with depth. We further demonstrate that each Pedogenon can be used to define SOC sequestration potential. Understanding SOC change can provide information on areas under SOC loss threat and require immediate remediation.
人类对土壤的影响,特别是在集约化农业方面,在过去200年中最为明显。在世界许多地区,集约化农业活动导致土壤有机碳(SOC)下降。然而,目前还缺乏能够从空间上估算人类活动对土壤有机碳变化的方法。在这里,我们使用土壤分型的概念将景观划分为土壤分型。在每个土壤区,我们取样了原生植被下和人类密集管理下的代表性土壤。我们调查了澳大利亚新南威尔士州纳莫依河谷下游地区(1700 km2),包括13个土壤区(土壤类别),并分析了99个土壤核的有机碳。利用数字土壤制图技术,利用土壤有机碳数据,利用环境协变量对土壤有机碳进行每10 cm至1 m的制图。利用原生植被下的采样点绘制原生状态下的SOC,所有数据均用于绘制当前状态下的SOC。通过比较两种状态(原生状态和当前状态)的SOC图,我们评估了SOC的变化。结果表明:灌溉区土壤有机碳损失最大,表层有机碳含量减少38%,其次为非灌溉区土壤有机碳损失30%,牧场土壤有机碳损失19%;所有种植区土壤有机碳含量均下降至少5 t C / ha - 1。表层土壤有机碳损失最大,随深度呈指数递减。我们进一步证明,每个Pedogenon都可以用来定义有机碳封存潜力。了解有机碳的变化可以提供受有机碳损失威胁的地区的信息,并需要立即采取补救措施。
AnthropoceneEarth and Planetary Sciences-Earth and Planetary Sciences (miscellaneous)
CiteScore
6.30
自引率
0.00%
发文量
27
审稿时长
102 days
期刊介绍:
Anthropocene is an interdisciplinary journal that publishes peer-reviewed works addressing the nature, scale, and extent of interactions that people have with Earth processes and systems. The scope of the journal includes the significance of human activities in altering Earth’s landscapes, oceans, the atmosphere, cryosphere, and ecosystems over a range of time and space scales - from global phenomena over geologic eras to single isolated events - including the linkages, couplings, and feedbacks among physical, chemical, and biological components of Earth systems. The journal also addresses how such alterations can have profound effects on, and implications for, human society. As the scale and pace of human interactions with Earth systems have intensified in recent decades, understanding human-induced alterations in the past and present is critical to our ability to anticipate, mitigate, and adapt to changes in the future. The journal aims to provide a venue to focus research findings, discussions, and debates toward advancing predictive understanding of human interactions with Earth systems - one of the grand challenges of our time.