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Effects of grazing intensity on soil carbon stocks following deforestation of a Hawaiian dry tropical forest

机译:夏威夷干旱热带森林砍伐森林后放牧强度对土壤碳储量的影响

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The effects of forest-to-pasture conversion on soil carbon (C) stocks depend on a combination of climatic and management factors, but factors that relate to grazing intensity are perhaps the least understood. To understand the long-term impact of grazing in converted pastures, methods are needed that accurately measure the impact of grazing on recent plant inputs to soil C in a variety of pasture management and climate settings. Here, we present an analysis from Hawai'i of changes in vegetation structure and soil organic carbon (SOC) along gradients of grazing intensity and elevation in pastures converted from dry tropical forest 100 years ago. We used hyperspectral remote sensing of photosynthetic vegetation, nonphotosynthetic vegetation (NPV) and exposed substrate to understand the effects of grazing on plant litter cover, thus, estimating recent plant inputs to soils (the NPV component). Forest-to-pasture conversion caused a shift from C3 to C4 plant physiology, thus the delta C-13 method was used in soil cores to measure the fraction of SOC accumulated from pasture vegetation sources following land conversion. SOC decreased in pasture by 5-9 kg C m(-2), depending upon grazing intensity. SOC derived from C3 (forest) sources was constant across the grazing gradient, indicating that the observed variation in SOC was attributable to changes in C inputs following deforestation. Soil C stocks were also reduced in pastures relative to forest soils. We found that long-term grazing lowers SOC following Hawaiian forest-to-pasture conversion, and that these changes are larger in magnitude that those occurring with elevation (climate). Further we demonstrate a relationship between remotely sensed measurements of surface litter and field SOC measurements, allowing for regional analysis of pasture condition and C storage where limited field data are available.
机译:从森林到草场的转化对土壤碳(C)库的影响取决于气候和管理因素的结合,但是与放牧强度有关的因素也许人们了解得最少。为了了解放牧对转基因牧场的长期影响,需要在各种牧场管理和气候环境下,准确测量放牧对最近植物输入土壤C的影响的方法。在这里,我们从夏威夷分析了100年前热带干旱林转换后的牧场中草场结构和土壤有机碳(SOC)沿放牧强度和海拔梯度的变化。我们使用光合植被,非光合植被(NPV)和裸露的底物的高光谱遥感来了解放牧对植物凋落物覆盖的影响,从而估算最近植物对土壤的投入(NPV成分)。从森林到牧场的转换导致植物C3向C4的转变,因此在土壤核心中使用了C-13增量法来测量土地转换后从草场植被源累积的SOC比例。牧场中的SOC降低了5-9 kg C m(-2),具体取决于放牧强度。从C3(森林)来源获得的SOC在整个放牧坡度上是恒定的,这表明观察到的SOC变化是由于森林砍伐后C输入的变化。相对于森林土壤,牧场中的土壤碳储量也减少了。我们发现,长期的放牧会降低夏威夷森林到牧草的转化后的SOC,并且这些变化的幅度大于海拔(气候)变化时的SOC。进一步,我们展示了遥感的地面垫料测量值与田间SOC测量值之间的关系,从而可以在有限的田间数据可用的情况下对牧场状况和C储存进行区域分析。

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