黑河中游荒漠绿洲区土地利用的土壤养分效应

土地利用影响地表覆被状况和生态过程,关系到土壤肥力与土壤碳库功能"源-汇"关系的改变。黑河中游甘州区和临泽县是我国西北干旱区典型的荒漠绿洲区,以土壤表层(0-20 cm)养分变化为对象,利用2011-2012年甘州区和临泽县的土壤野外调查数据和该区全国第二次土壤普查数据,对两时期土壤表层养分(土壤有机质、全氮、全磷、全钾及pH值)的变化特征进行比较研究。结果表明:研究区土壤有机质、全磷含量分别降低了3.54%和12.5%;而全氮、全钾和pH值分别增加了74.4%、98.2%和4.9%。全国第二次土壤普查时期,荒漠、耕地与草地三者在各土壤养分上没有显著差异,但林地在土壤有机质、全氮、全钾上显著高于前三者。2011-2012年,耕地土壤的全磷、全氮与其它土地利用存在显著差异。土地利用的保持和改变对土壤养分变化有着重要影响,耕地的长期耕作使得土壤有机质含量降低4.94%,全氮增加86.93%,全磷减少5.02%,土壤碱性增强;荒漠植被的自然演替使土壤有机质含量增加66.21%,全氮增加71.70%,全磷含量减少37.33%,土壤碱性变弱。所以,耕地扩张及其长期耕作活动将导致地力退化并有盐碱化风险,而荒漠等自然生态系统保护有利于土壤肥力的改善和土壤固碳功能的发挥。     

社会经济系统磷物质流分析--以安徽省含山县为例

氮、磷等营养物质过量输入是造成我国湖泊富营养化问题日益严重的根源,磷作为水体富营养化过程关键限制元素,主要来自流域社会经济系统中的人类活动排放,因此,定量刻画社会经济系统内的磷流动路径是追踪水体外源磷来源和进行有效控制磷排放量的前提。以巢湖流域的安徽省含山县为例,构建社会经济系统磷流分析框架,建立磷流核算模型,并在实地调查和数据统计分析的基础上定量刻画了含山县2008年度社会经济系统磷流路径。结果表明,2008年含山县社会经济系统向水体排放的磷总量为1592t,其中农业种植子系统的排放所占比例最大(77%),该子系统的磷利用效率也较低(45%)。因此,含山县富营养化治理的重点是优化农业种植系统的磷流路径,主要措施包括合理施肥、科学排灌等。     

Mineralization, pore water chemistry and phosphorus release from peaty sediments in the eutrophic Loosdrecht lakes, The Netherlands

SUMMARY. 1. Pore water chemistry in peaty sediment was monitored for a year at two representative locations of the eutrophic shallow Loosdrecht lakes. The Netherlands. Phosphorus fluxes over the sediment-water interface were calculated using measured concentration gradients in the pore water and compared to fluxes measured under laboratory conditions. Results were analysed with Redundancy Analysis to detect patterns of variation in pore water chemistry and in measured and calculated fluxes, that could be ascribed to environmental variables.
2. It was demonstrated that phosphorus fluxes measured in long-term laboratory incubations were not correlated to any of the pore water characteristics.
3. Initial phosphorus fluxes measured in sediment columns, which varied between −7.7 and 1330 μmol m⁻²: day⁻¹, were correlated significantly to the calculated phosphorus flux over the sediment-water interface.
4. The high correlation between calculated fluxes of ammonia, phosphorus and methane and measured initial flux of phosphorus, conclusively pointed to mineralization of organic matter as the driving force for phosphorus release from the sediment.
5. Redundancy Analysis demonstrated that the rates of mineralization and phosphorus release were only weakly related to temperature. They appeared to be especially stimulated by the autumnal decrease in temperature which was probably related to an extra input of organic matter.     

Accuracy assessments of the GLOBCOVER dataset using global statistical inventories and FLUXNET site data

The spatio-temporal distribution of land cover provides fundamental data for global climate and environmental change research. In recent decades, five global land cover maps have been produced based on remote sensing data sources and methodologies. Related research have shown that the availability and quality of the first four global land cover datasets are poor at the regional or the continental scale for a variety of reasons. There is still no consensus on the accuracy of the latest global land cover map. Based on comparison of the land cover dataset with the statistical cropland data from FAO and the FLUXNET site data, this paper discusses the accuracy of the fifth global land cover map, namely, the GLOBCOVER dataset, at different spatial scales. At the global scale, the cropland area obtained from the GLOBCOVER dataset is greater than that of the FAO statistical data by 47.06–84.49%, and the land cover types of the GLOBCOVER dataset have a 65.02% consistency with that of the FLUXNET site data. At the continental scale, the difference between cropland areas obtained from the GLOBCOVER dataset and the statistical cropland area vary from ?43.42% to 502.36%; continents that have a more accurate cropland area compared to the FAO statistical data tend to be less consistent with the FLUXNET site data. In general, North America has a higher accuracy and Oceania has a lower accuracy. At the country scale, the accuracy estimates vary sharply over a wide range: between ?100.00% and 190670.37%. It is recommended that future studies should pay careful attention to the data validation step before using the GLOBCOVER dataset for any particular problem. Future studies are also required for the development of a universal land cover classification system and advanced algorithms for remote sensing classification of global land cover maps.     

我国农田生态系统重金属的循环与调控

本文系统分析了我国农田土壤重金属的含量状况,探讨了农田生态系统中重金属的输入、输出及其平衡.农田生态系统中重金属存在一定的累积效应,但整体上超标风险较小,而部分作物、特别是蔬菜可能存在一定的超标风险.在采矿区和冶炼厂周边地区,以及废弃物利用强度较大的农区,土壤和作物中重金属超标的风险较大,是普通农区的十倍甚至数十倍以上.针对我国农田重金属污染现状,提出了调控农田生态系统重金属循环的有效措施,并对相关领域今后的研究进行了展望.     

Mapping global cropland and field size

A new 1 km global IIASA‐IFPRI cropland percentage map for the baseline year 2005 has been developed which integrates a number of individual cropland maps at global to regional to national scales. The individual map products include existing global land cover maps such as GlobCover 2005 and MODIS v.5, regional maps such as AFRICOVER and national maps from mapping agencies and other organizations. The different products are ranked at the national level using crowdsourced data from Geo‐Wiki to create a map that reflects the likelihood of cropland. Calibration with national and subnational crop statistics was then undertaken to distribute the cropland within each country and subnational unit. The new IIASA‐IFPRI cropland product has been validated using very high‐resolution satellite imagery via Geo‐Wiki and has an overall accuracy of 82.4%. It has also been compared with the EarthStat cropland product and shows a lower root mean square error on an independent data set collected from Geo‐Wiki. The first ever global field size map was produced at the same resolution as the IIASA‐IFPRI cropland map based on interpolation of field size data collected via a Geo‐Wiki crowdsourcing campaign. A validation exercise of the global field size map revealed satisfactory agreement with control data, particularly given the relatively modest size of the field size data set used to create the map. Both are critical inputs to global agricultural monitoring in the frame of GEOGLAM and will serve the global land modelling and integrated assessment community, in particular for improving land use models that require baseline cropland information. These products are freely available for downloading from the http://cropland.geo-wiki.org website.     

The release of nutrients and organic matter from aquaculture systems in Nordic countries

The extent of the environmental impact of an aquaculture development is mainly dependent on husbandry, feeding technique, feed composition and site selection. Feed composition, digestibility and feed conversion coefficient are of paramount importance for the level of discharge of wastes derived from fish farming. These determine the release of nutrients (e.g. phosphorus and nitrogen) and organic material. Excretion products (in particular waste feed and faeces) may cause changes in the ecosystem. However, the overall environmental load derived from aquaculture is comparatively small when compared to other waste loads from communities, industries, agriculture and forestry. The amount of phosphorus and nitrogen in feeds has decreased to 1 % and 7%, respectively, while feed conversion efficiency due to high energy feeds has improved to values around 1.2 in most salmon farming operations. This has greatly reduced overall environmental loads, which are presently calculated with 10 kg phosphorus and 60 kg nitrogen per tonne of fish produced. The organic wastes per tonne produced are presently estimated to reach 2500 kg wet weight per tonne live weight fish. System design and site selection are additional important considerations which influence greatly the level of environmental impact. The advantage of land-based systems over water-based systems is the fact that water treatment of effluents is possible in such systems, thereby greatly reduction total loads to receiving waters. The paper mainly focusses on nutritional aspects of environmental load.     

MELODIE: a whole-farm model to study the dynamics of nutrients in dairy and pig farms with crops

In regions of intensive pig and dairy farming, nutrient losses to the environment at farm level are a source of concern for water and air quality. Dynamic models are useful tools to evaluate the effects of production strategies on nutrient flows and losses to the environment. This paper presents the development of a new whole-farm model upscaling dynamic models developed at the field or animal scale. The model, called MELODIE, is based on an original structure with interacting biotechnical and decisional modules. Indeed, it is supported by an ontology of production systems and the associated programming platform DIESE. The biotechnical module simulates the nutrient flows in the different animal, soil and crops and manure sub-models. The decision module relies on an annual optimization of cropping and spreading allocation plans, and on the flexible execution of activity plans for each simulated year. These plans are examined every day by an operational management sub-model and their application is context dependent. As a result, MELODIE dynamically simulates the flows of carbon, nitrogen, phosphorus, copper, zinc and water within the whole farm over the short and long-term considering both the farming system and its adaptation to climatic conditions. Therefore, it is possible to study both the spatial and temporal heterogeneity of the environmental risks, and to test changes of practices and innovative scenarios. This is illustrated with one example of simulation plan on dairy farms to interpret the Nitrogen farm-gate budget indicator. It shows that this indicator is able to reflect small differences in Nitrogen losses between different systems, but it can only be interpreted using a mobile average, not on a yearly basis. This example illustrates how MELODIE could be used to study the dynamic behaviour of the system and the dynamic of nutrient flows. Finally, MELODIE can also be used for comprehensive multi-criterion assessments, and it also constitutes a generic and evolving framework for virtual experimentation on animal farming systems.     

Global Phosphorus Flows in the Industrial Economy From a Production Perspective

Human activity has quadrupled the mobilization of phosphorus (P), a nonrenewable resource that is not fully recycled biologically or industrially. P is accumulated in both water and solid waste due to fertilizer application and industrial, agricultural, and animal P consumption. This paper characterizes the industrial flows, which, although smaller than the agricultural and animal flows, are an important phosphorus source contributing to the pollution of surface waters. We present the quantification of the network of flows as constrained by mass balances of the global annual metabolism of phosphorus, based on global consumption for 2004, all of which eventually ends up as waste and in the soil and water systems. We find that on a yearly basis, 18.9 million metric tons (MMT) of P is produced, of which close to 75% goes to fertilizer and the rest to industrial and others uses. Phosphoric acid is the precursor for many of the intermediate and end uses of phosphate compounds described in this study and accounts for almost 80% of all P consumed. Eventually, all of the P goes to waste: 18.5 MMT ends up in the soil as solid waste, and 1.32 MMT is emissions to air and water. Besides quantifying P flows through our economy, we also consider some possible measures that could be taken to increase the degree of recovery and optimization of this resource and others that are closely related, such as the recovery of sulfur from gypsum and wastewater (sludge), and fluorine from wet phosphoric acid production.     

The influence of farming technique on cropland: A new approach for the Ecological Footprint

The relationship between farming management and the overexploitation of natural resources is often a theme of discussion in the environmental sciences. Moreover, farmers’ choices – driven by consumer demand – have a significant effect on the agricultural production system.The Ecological Footprint methodology as it currently implemented assumes that all cropland activities are sustained by the capacity of the ecosystem, basing both demand and capacity calculations on the exact same flow accounting. This causes some confusion in the evaluation of the ecological performance of farming because it appears that this activity has no consequences on the planet.This paper proposes a solution to this duality caused by the current methodological assumption about croplands, and investigates the influence of different farming techniques on Ecological Footprint results. Starting from the concept of an embodied footprint in production, we propose a new approach for the evaluation of farming performance. This approach permits an estimation of the impact of farming activity, linked to the farmers’ technique, and a calculation of the crop Footprint in reference to the production capacity of the natural system.Building on the central methodology of the Ecological Footprint, we provide a different evaluation system and show case study results for comparison.     

磷元素物质流分析研究进展

磷是重要的营养元素,也是不可再生的重要非金属矿物资源。为了分析人类活动对磷流动的扰动,国内外开展了大量磷元素的物质流分析和模拟。综述了磷元素物质流分析的最新研究进展,分析了国内外磷元素物质流研究的特点和不足,并展望了未来相关研究的研究热点和发展方向。从研究尺度看,现有磷元素的物质流研究以全球尺度和国家尺度为主,区域和城市尺度以及企业和产品尺度的研究较少。从研究问题看,现阶段研究主要关注农业或者食品生产和消费对磷流动的影响,对林业、钢铁和能源部门略有涉及。从模型特征看,现有研究以分析流量变化的静态模型为主,考虑存量变化的动态模拟较少。从研究的发展方向看,未来磷物质流的相关分析将关注五大问题:(1)考虑不同驱动力和存量变化的动态模拟;(2)不同层次和尺度的磷足迹研究;(3)磷与其他元素相比对社会经济的重要性;(4)全球变化背景下不同部门磷依赖的脆弱性;(5)磷和其他元素的耦合研究。为了适应未来的研究需求,磷的物质流模拟重点在于开发动态模型,并将物质流分析与多种手段结合,以预测全球变化、社会经济发展、技术变化以及其他重要变化对磷流动的扰动及其相应的环境影响。     

Unravelling the anthropogenic pathways of phosphorus in the food production and consumption system of Bangladesh through the lens of substance flow analysis

Phosphorus (P) is central to food production. Current understanding about the global phosphorus system is dominated by studies in wealthier nations where soil fertility, fertilizer supply chains, and agronomic tracking have long been established. In contrast, developing nations are experiencing major agricultural transitions and the associated phosphorus flows remain a significant knowledge gap. We compiled and analyzed several years of recent agricultural datasets for Bangladesh, currently the eighth most populous nation, using substance flow analysis for phosphorus. From 2000 to 2016, rice production increased by >50% and remained the dominant crop with remarkably higher phosphorus flow (49.96 kt in 2016) than all other crops. Phosphorus content of livestock products in 2016 exceeded 6.00 kt, more than double in the year 2000, driven primarily by phosphorus in milk and secondarily in meat/eggs. These agricultural changes coincided with a doubling of national phosphorus fertilizer consumption since 2000, a fourfold increase since the global food crisis (2009), and a pronounced rise in the phosphorus import dependency ratio, which was the highest among all countries compared. In turn, during 2010s fertilizer phosphorus use exceeded phosphorus as food + feed production leading to soil phosphorus accumulation, and loss as burned manure became one of the largest phosphorus flows in the entire system, equivalent to half of fertilizer use. This dramatic reconfiguration of the Bangladesh phosphorus system illustrates an important case of agricultural expansion and intensification that is still playing out, with similar situations occurring in developing nations where population growth rates are high, and access to commercial fertilizers has risen.     

农田土壤中磷素有效性及影响因素

土壤中磷的有效性直接决定着农田生产力. 基于分布于我国不同气候区长期定位施肥试验,总结了不同农田土壤的磷素含量、有效性及转化的影响因素.结果表明： 目前我国不同类型的土壤中全磷含量在0.31～1.72 g·kg^-1,速效磷含量在0.1～228.8 mg·kg^-1.土壤母质、理化性质和施肥方式是影响农田土壤磷素有效性的主要因素,未来应注重有机肥和化肥的混合施用以提高农田土壤磷素有效性,并关注可能导致的环境影响.     

Regionally differentiated estimates of cropland N2O emissions reduce uncertainty in global calculations

Nitrogen (N) additions to cropland soils are the largest source of anthropogenic nitrous oxide (N₂O) emissions and are an important contributor to global greenhouse gas radiative forcing. Progress in understanding controls on N₂O fluxes from soils is demonstrated in increasingly sophisticated emissions estimates with improved spatial and source resolution. These methods build upon ongoing field, laboratory, and modeling advances that are restricted to just a handful of countries. Thus, burgeoning new knowledge is of limited utility for improving N₂O emissions estimates for the rest of the world where prospects for near‐term advances are constrained by the limited breadth of observations and availability of model driver data. Here, we use Bayesian inversion to leverage information from recent national‐level N₂O emission inventories and reduce uncertainty by up to 65% for estimates of regional and global direct cropland N₂O emissions. Our estimates for the proportion of N inputs lost as N₂O vary by a factor of two between regions and depart from existing default emission factors, yet regional emissions estimates based on these factors are consistent with global, regional, and local observations. Improved regional emission factors will enhance national greenhouse gas inventories in information‐poor countries and guide efforts to reduce agricultural N₂O emissions.     

Impacts of mussel (<Emphasis Type="Italic">Mytilus galloprovincialis</Emphasis>) farming on oxygen consumption and nutrient recycling in a eutrophic coastal lagoon

Fluxes of oxygen, nitrogen and phosphorus were determined in two areas of the Sacca di Goro lagoon, at a site influenced by the farming of the mussel Mytilus galloprovincialis and a control site. Mussel farming induced intense biodeposition of organic matter to the underlying sediments, which stimulated sediment oxygen demand, and inorganic nitrogen and phosphorus regeneration rates compared to the nearby control station. Overall benthic fluxes (–11.4 ± 6.5 mmol O₂ m⁻² h⁻¹; 1.59 ± 0.47 mmol NH₄⁺ m⁻² h⁻¹ and 94 ± 42 μmol PO₄³⁻ m⁻² h⁻¹) at the mussel farm are amongst the highest ever recorded for an aquaculture impacted area and question the belief that farming of filter-feeding bivalves has inherently lower impacts than finfish farming. In situ incubations of intact mussel ropes demonstrated that the mussel rope community was an enormous sink for oxygen and particulate organic matter, and an equally large source of dissolved inorganic nitrogen and phosphate to the water column. Overall, a one meter square area of␣mussel farm (mussel ropes and underlying sediment) was estimated to have an oxygen demand of 46.8 mmol m² h⁻¹ and to regenerate inorganic nitrogen and phosphorus at rates of 8.5 and 0.3 mmol m² h⁻¹, with the mussel ropes accounting for between 70 and more than 90% of the overall oxygen and nutrient fluxes. Even taking into account that within the farmed area of the Sacca di Goro lagoon, there are 15–20 m⁻² of open water for each one covered with mussel ropes, the mussel ropes would account for a large and often dominant part of overall oxygen and nutrient fluxes. These results demonstrate that it is essential to take into account the activity of the cultivated organisms and their epiphytic community when assessing the impacts of shellfish farming. Overall, whilst grazing by the mussel rope community could act as a top-down control on the phytoplankton, most of the ingested organic matter is rapidly recycled to the water column as inorganic nutrients, which would be expected to stimulate phytoplankton growth. Consequently, the net effect of the mussel farming on phytoplankton dynamics, may be to increase phytoplankton turnover and overall production, rather than to limit phytoplankton biomass.     

土地利用/覆盖变化对陆地生态系统碳循环的影响

土地利用/覆盖变化是学术界最为关注的环境变化问题之一,它能够影响陆地生态系统的生物多样性、水、碳和养分循环、能量平衡,引起温室气体释放增加等其它环境问题。不同类型的土地利用/覆盖变化对生态系统碳循环的作用不同,由高生物量的森林转化为低生物量的草地、农田或城市后,大量的CO₂将释放到大气中。全球土地利用/覆盖变化具有很强的空间变异性,对生态系统碳循环的影响同样具有明显的空间差异:热带地区的土地利用/覆盖变化造成大量的碳释放,而中高纬度地区土地利用/覆盖变化则表现为碳汇。目前,土地利用/覆盖变化引起的生态系统碳循环变化主要是通过模型模拟来估算的。尽管土地利用/覆盖变化及其相关过程与生态系统碳循环的关系已经比较清楚,但是,由于土地利用/覆盖变化过程复杂且影响广泛,对于如何量化两者之间的关系还存在很多不确定性。目前的量化过程主要是利用经验数据来实现的,机理性不强,使得对土地利用/覆盖变化造成的陆地生态系统CO₂释放量的估测差异很大。除了进一步加强长期定位研究以获得土地利用/覆盖变化与生态系统碳循环过程的定量关系外,土地利用/覆盖变化模型与植被动态模型、生态系统过程模型的耦合也是今后模型发展的主要方向之一。采用合理的管理措施能够大量增加土地利用/覆盖变化过程中的碳储存量,降低碳释放量,因此在模型中耦合管理措施来研究土地利用/覆盖变化过程对生态系统碳循环的影响是未来几年的工作重点。     

Fluxes and retention of sediment and nutrients in valley bottom fish and rice farms and wetlands: impacts on surface water

This study compares nutrient and sediment retention among rice and fish farms and wetlands in valley bottoms in southern Rwanda. Small-scale wetland, rice and fishpond experimental systems were established to measure sediment, nitrogen (N) and phosphorus (P) fluxes during a 9-month period. There were significant differences in the processes contributing to sediment, N and P retention in the three systems related to system characteristics, management practices, and seasons. Overall nutrient retention was higher in the rice and fish systems, but these systems had higher inputs and outputs of sediment and nutrients. In rice plots, resuspension and discharge of sediment and nutrients to the outflow were caused by ploughing and weeding during the first 3 months of the culture period. In fishponds, nutrients and sediment discharge were associated with water renewal and sediment removal during the last 5 months of the farming period. The undisturbed wetland plots had the lowest outflows of sediment and nutrients. Nutrient uptake and accumulation in biomass was much higher in rice and wetland vegetation than in fish biomass. In fishponds and wetlands, nutrients accumulated in soil, whereas rice plots showed a decrease or depletion in nutrient storage. To increase nutrient utilization at the plot level, sediment and nutrient discharge from land preparation and rice transplanting should be reduced by better farm practices. Within a catchment, nutrient flows can be integrated by using fishpond sediments for crop farming, by incorporating natural wetlands in crop rotations or using them as buffer zones.

     

Groundwater and pore water inputs to the coastal zone

Both terrestrial and marine forces drive underground fluid flows in the coastal zone. Hydraulic gradients on land result in groundwater seepage near shore and may contribute to flows further out on the shelf from confined aquifers. Marine processes such as tidal pumping and current-induced pressure gradients may induce interfacial fluid flow anywhere on the shelf where permeable sediments are present. The terrestrial and oceanic forces overlap spatially so measured fluid advection through coastal sediments may be a result of composite forcing. We thus define “submarine groundwater discharge” (SGD) as any and all flow of water on continental margins from the seabed to the coastal ocean, regardless of fluid composition or driving force. SGD is typically characterized by low specific flow rates that make detection and quantification difficult. However, because such flows occur over very large areas, the total flux is significant. Discharging fluids, whether derived from land or composed of re-circulated seawater, will react with sediment components. These reactions may increase substantially the concentrations of nutrients, carbon, and metals in the fluids. These fluids are thus a source of biogeochemically important constituents to the coastal ocean. Terrestrially-derived fluids represent a pathway for new material fluxes to the coastal zone. This may result in diffuse pollution in areas where contaminated groundwaters occur. This paper presents an historical context of SGD studies, defines the process in a form that is consistent with our current understanding of the driving forces as well as our assessment techniques, and reviews the estimated global fluxes and biogeochemical implications. We conclude that to fully characterize marine geochemical budgets, one must give due consideration to SGD. New methodologies, technologies, and modeling approaches are required to discriminate among the various forces that drive SGD and to evaluate these fluxes more precisely.     

Effect of Erosion on Productivity in Subtropical Red Soil Hilly Region: A Multi-Scale Spatio-Temporal Study by Simulated Rainfall

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.     

Global Life Cycle Paper Flows,Recycling Metrics,and Material Efficiency

Despite major improvements in recycling over the last decades, the pulp and paper sector is a significant contributor to global greenhouse gas emissions and other environmental pressures. Further reduction of virgin material requirements and environmental impacts requires a detailed understanding of the global material flows in paper production and consumption. This study constructs a Sankey diagram of global material flows in the paper life cycle, from primary inputs to end‐of‐life waste treatment, based on a review of publicly available data. It then analyzes potential improvements in material flows and discusses recycling and material efficiency metrics. The article argues that the use of the collection rate as a recycling metric does not directly stimulate avoidance of virgin inputs and associated impacts. An alternative metric compares paper for recycling (recovered paper) with total fibrous inputs and indicates that the current rate is at just over half of the technical potential. Material efficiency metrics are found to be more useful if they relate to the reuse potential of wastes. The material balance developed in this research provides a solid basis for further study of global sustainable production and consumption of paper. The conclusions on recycling and efficiency should be considered for improving environmental assessment and stimulating a shift toward resource efficiency and the circular economy.