三高农业与土肥

三高农业与土壤和肥料有密切的关系。地力是作物产量的重要基础,要取得高产,就必须坚持不懈地培肥地力。综合地力、土壤中营养元素及有害或有毒物质的含量、肥料类型和施肥技术,都对农产品的品质有很大的影响。要提高农产品的产量和质量,就要因土种植,合理施肥。高产优质是经济效益的主要构成因素,因而,培肥地力、因土种植、合理施肥能提高经济效益。忽视土肥工作,将影响三高农业的发展。     

The agricultural impact of opencast coal mining in England and Wales

Opencast coal mining in England and Wales can cause a wide range of environmental problems which are increasingly public issues due to the planned expansion in output and the impact this may have on agriculture and landscape. Opencast mining is reviewed on a county by county basis to identify the variations in the disturbance caused. A detailed review of restoration techniques and the agricultural quality of the restored land is presented, and the role of Planning Authorities is discussed. Significant variations in the impact of opencast operations are identified, especially in relation to the potential for derelict land reclamation and the grade of agricultural land affected. The latter is generally lower grade 3 and below, although in certain areas operations are entering land of higher agricultural and scenic quality. The quality of restoration, while good, still has scope for improvements, such as reducing soil compaction and the subsequent management of the land by the farmer. The impact on agricultural productivity is difficult to assess, but it appears to be only slight in those cases where recent restoration techniques were used and when lower grade agricultural land is taken.     

森林土地利用变化及其对碳循环的影响

由于人口剧增，人类活动的影响不断加大，在过去100年全球土地利用／土地覆被发生了巨大的变化。最常见的土地利用变化是由森林转变为农业用地。森林砍伐使森林生态系统地上部生物量大大减少，砍伐后作农业用地，降低了植被生产力，减少了土壤有机质的输入，增强了腐殖质的矿化作用，有机质分解速率增加，有机碳贮量随之降低，从而影响到森林生态系统的碳循环，使大量碳元素释放到大气中，引起温室效应，导致全球变暖。另一个常见的土地利用变化是植树造林和森林恢复，这一过程可以增加森林生态系统的碳储量，从而减缓大气CO2体积分数的上升。     

加拿大最佳管理措施流域评价项目评述

可持续农业的目的是在保持良好环境质量的同时获得较高的农业生产率。最佳管理措施(BMPs)在世界范围内已得到广泛应用,以减少农业污染物对水环境的影响。自2004年以来,加拿大农业部实施了最佳管理措施流域评价(WEBs)项目,在全国各地选择了有代表性的9个小流域,对BMPs的环境和经济效益进行评价。笔者对过去几年来WEBs项目的进展、研究方法及主要成果进行简要的回顾,并对在中国开展类似项目的必要性和启示进行了探讨。     

喀斯特石漠化生态系统恢复演替过程中土壤质量特性研究——以广西都安县澄江小流域为例

采用空间序列代替时间序列的方法,以广西都安县澄江小流域为例,研究广西喀斯特山区石漠化生态系统恢复演替过程中土壤质量的变化特征.在研究区内选择石漠化恢复演替的8个阶段,即石漠化土地、坡耕地、矮草丛、高草丛、灌草丛、灌丛、人工恢复乔木林、自然恢复乔木林的典型样地,对土壤化学和生物学性状进行了比较研究,以探讨石漠化生态系统恢复演替过程中土壤质量的修复状况.结果表明:不同的演替阶段导致了土壤化学和生物学性质的显著差异,而且在植被向更高一级阶段发展过程中土壤各项指标都得到提高,土壤质量总体呈现改良的态势.随着植被演替的正向进行,土壤质量指数呈增长趋势,不同演替阶段土壤质量综合指数分别为:石漠化土地,134.78;坡耕地,192.24;矮草丛,235.18;高草丛,260.67;灌草丛,317.89;灌丛,359.80;人工恢复乔木林,363.39;自然恢复乔木林,460.77.自然植被的正向演替是提高土壤质量的有效途径,恰与石漠化过程相反.     

Influence of slope aspect on soil physico-chemical and biological properties in the mid hills of central Nepal

This study assessed the influence of slope aspect and land use on soil physio-chemical and biological properties (soil quality indicators) on contiguous south- and north-facing slopes of the mid hills in central Nepal, having the same climate, vegetation and parent material. In each aspect, two treatments (agriculture and forest) were chosen and four replicates taken for each treatment. Soil sample collection and microarthropod extraction was done according to the standard methodology: soil core samples (10 × 10 × 5 cm) and extraction with the modified Berlese–Tullgren funnel. The investigated soil variables were temperature, moisture, faunal abundance and diversity, organic matter, organic carbon, bulk density and pH. Except in a few cases, all considered soil properties showed significant differences between aspects and land use. Soils of the north-facing slope had higher SOC content, moisture, faunal abundance and diversity, and lower temperature and pH. Variations due to topographic aspect induced varied microclimates, causing differences in faunal abundance and diversity; soil moisture, temperature and organic matter trends affected soil fertility and ultimately soil quality. Further studies are required to clarify the complex interactions between soil properties (physio-chemical and biological), vegetation and slope aspect in Nepal, as well as to develop soil biological indicators as a tool to assist in sustainable land management.     

Examining the relationship between ecosystem structure and function using structural equation modelling: A case study examining denitrification potential in restored wetland soils

An ongoing debate in ecology is the relationship between community or ecosystem structure and function. This relationship is particularly important in restored ecosystems because it is often assumed that restoring ecosystem structure will restore ecosystem functioning, but this assumption is frequently not tested. In this study, we used a novel application of structural equation modelling (SEM) to examine the relationship between ecosystem structure and function. To exemplify how to apply SEM to explore this relationship, we used a case study examining soil controls on denitrification potential (DNP) in two restored wetlands. Our objectives were to examine (1) whether both restored wetland soil ecosystems had similar relationships among soils variables (i.e. similar soil ecosystem structure) and (2) whether the soil variables driving denitrification potential (DNP) were similar at both sites (i.e. the soil ecosystems were functioning in a similar manner). Using the unique ability of SEM to test model structure, we proposed a SEM to represent the soil ecosystem and tested this structure with field data. We determined that the same model structure was supported by data from both systems suggesting that the two restored wetland systems had similar soil ecosystem structure. To test whether both ecosystems were functioning in a similar way, we examined the parameters of each model. We determined that the drivers of DNP function were not the same at both sites. Higher soil organic matter was the most important predictor of higher DNP at both sites. However, the other significant relationships among soils variables were different at each system indicating that the soils were not functioning in exactly the same way at each site. Overall, these results suggest that the restoration of ecosystem structure may not necessarily ensure the restoration of ecosystem functioning. In this study we capitalize on an inherent feature of SEM, the ability to test model structure, to test a fundamental ecological question. This novel approach is widely applicable to other systems and improves our understanding of the general relationship between ecosystem structure and function.     

大冶矿区土壤重金属积累对土壤酶活性的影响

大冶矿区位于湖北省的东南部,是我国的青铜之乡,长期的采矿和冶炼活动已使该矿区土地生产力和农产品品质严重下降。为了探明相关重金属的污染状况,应用野外调查与采样分析相结合的方法,研究了大冶矿区土壤酶活性和土壤中重金属的累积特性。结果表明:矿区土壤Cu、Pb、Zn、Cd、As全量的平均值分别是该区土壤背景值的35.1倍、16.0倍、3.0倍、29.8倍、1.1倍。不同样点土壤酶活性存在一定程度的差异。土壤重金属胁迫对土壤酶活性主要表现为抑制作用,其中对土壤重金属响应较敏感的酶为脲酶和过氧化氢酶,这两种酶与重金属Cu、Pb、Zn、Cd、As的全量分别呈显著或极显著的负相关。这些研究结果对于大冶矿区土壤环境质量评价及生态修复有一定的指导意义。     

Microbial community variation and its relationship with nitrogen mineralization in historically altered forests

Past land use can impart soil legacies that have important implications for ecosystem function. Although these legacies have been linked with microbially mediated processes, little is known about the long-term influence of land use on soil microbial communities themselves. We examined whether historical land use affected soil microbial community composition (lipid profiles) and whether community composition was related to potential net nitrogen (N) mineralization rates in southern Appalachian (USA) forest stands abandoned from agriculture or logging and reforested >50 yr ago. Microbial community composition was determined by a hybrid procedure of phospholipid fatty acid (PLFA) and fatty acid methyl ester (FAME) analysis. We found that community composition varied significantly with past land use. Communities in formerly farmed stands had a higher relative abundance of markers for gram-negative bacteria and a lower abundance of markers for fungi compared with previously logged and reference (i.e., no disturbance history) stands. Potential net N mineralization rates were negatively correlated with fungal and gram-negative bacterial markers in both farmed and reference stands, and fungal abundance and soil bulk density effectively predicted mineralization rates in all stands. Our results indicate that the alteration of microbial communities by historical land use may influence the ecosystem processes they mediate. This is in contrast to typical expectations about microbial community resilience to change. Here, the decrease in fungal abundance observed from disturbance appeared to result in decreased nitrogen mineralization over the long term.     

不同恢复年限退化土壤有机氮组分变化特征

为明确退化土壤在不同恢复年限下土壤有机氮组分变化规律,以福建长汀县退化红壤为研究对象,利用时空替代法,选取5个典型的不同植被恢复阶段样地,分别为裸地,恢复7、17、23、35 a的马尾松(Pinus massoniana)人工林,采用Bremner酸水解法研究土壤有机氮各组分的变化特征.结果表明,与裸地相比,恢复年限为...     

Negative Off‐Site Impacts of Ecological Restoration: Understanding and Addressing the Conflict

Abstract: Ecological restoration is a key component of biological conservation. Nevertheless, unlike protection of existing areas, restoration changes existing land use and can therefore be more controversial. Some restoration projects negatively affect surrounding landowners, creating social constraints to restoration success. Just as negative off‐site impacts (i.e., negative externalities) flow from industrial areas to natural areas, restoration projects can generate negative externalities for commercial land uses, such as agriculture. Negative externalities from industry have led to government regulation to prevent human health and environmental impacts. Negative externalities from restoration projects have elicited similar legal constraint on at least one large‐scale conservation project, riparian restoration in the Sacramento River Conservation Area. The negative externalities of restoration that are perceived to be the direct result of specific goals, such as endangered species management, are likely to be more contentious than externalities arising from unintended phenomena such as weed invasion. Restoration planners should give equal consideration to off‐site characteristics as to on‐site characteristics when choosing sites for restoration and designing projects. Efforts to control externalities can lead to off‐site ecological benefits.     

不同利用方式下吴江市耕地土壤环境质量变化

土地利用方式的不同影响着土壤环境质量的变化。文章采用了2003年江苏省吴江市耕地质量监测中资料,分析了6种不同土地利用方式下的土壤养分及Pb、Cr、Hg、As、Cd等5种重金属元素全量的变化,并采用土壤质量综合指数(SQI)法计算不同利用下的土壤环境质量指数。结果表明:近20多年来,吴江市土地利用方式发生了明显的变化,这种变化对本土壤养分和重金属含量产生了十分明显的影响。在稻田、林地、桑园、菜地、果园、旱地六种吴江常见的土地利用方式中,稻田土壤环境质量综合指数显著高于其他利用下,而其他五种利用方式下土壤质量的差别不明显。可见稻田不仅是一种太湖地区传统的利用方式,更是保持环境质量相对最佳的土地利用方式。     

Analytik von Mineralölkohlenwasserstoffen: Die Problematik der Probenaufbereitung

For the determination of mineral oil hydrocarbons in water and soil, IR-as well as GC/FID-methods (DEV H-18, ISO/TR 11046, NEN 5733) are used. Independent of the measurement method, different clean-up procedures are prescribed in these standard methods. Aluminium oxide, silica gel and magnesium silicate (Florisil^®) are used as adsorbents. This article describes the problems of clean-up occurring in mineral oil analysis using selected substances. Tests concerning the type of adsorbent, extract medium, clean-up-technique and extract/adsorbent-ratio are presented. It will be shown that the clean-up procedure has to be counted as a significant factor of influence in the determination of mineral oil hydrocarbons. The sources of errors resulting from clean-up as well as the possibilities to avoid them are presented. An extraction solvent for soils which is simple to handle and optimally adjustable to the requirements of the clean-up procedure is presented.     

Vermiculite addition to soil decreases N water pollution by over 30%

The large amounts of nitrogen-containing mineral fertilisers in industrial agriculture are leading to water pollution with effects such as eutrophication and death of aquatic life. There is therefore a need for techniques to keep N in the soil to prevent leaching in waters. Here, we tested the effect of the addition of vermiculite, a phyllosilicate mineral, to the soil, on fertiliser NH₄ ⁺-N retention in laboratory experiments during 14–45 days. The added amount of vermiculite was twice the amount of the nitrogen fertilizer added. Our results show that addition of vermiculite increases NH₄ ⁺-N retention by over 30%, compared to a control. Adding vermiculite is thus a promising technique to control the eutrophication of water systems as well as reducing agriculture cost.     

耕地土壤碳固存的措施与潜力

土壤CO2排放与土壤退化、土壤有机质(SOC)含量减少和土壤质量下降密切相关。耕地具有较大的碳固存潜力。通过采用最佳管理措施(BMPs)和进行土壤修复来提高土壤质量，能增加SOC含量和提高土壤生产力，并能部分起到减缓温室效应的作用。文章从土壤固碳的机制入手，系统总结了在耕作土壤碳固存方面的研究。从土壤侵蚀控制、退化土壤修复、保护性耕作、残落物管理，改善农作物制度等方面，论述了耕地的固碳潜力，并提出了一系列实现碳固存的措施。最后估算出耕地土壤总的固碳潜力为0．73～0．87Pg/a。研究表明,在替代性能源开发之前，耕地碳固存是一项切实可行的措施。     

Trace metals in the coastal soils developed from estuarine floodplain sediments in the Croatian Mediterranean region

Fertile soils in the River Neretva estuary were developed by fluvial sedimentation and deposition of the eroded soil material from the karst hills within the catchment. After extensive reclamation, two reclaimed land zones (fluvial terraces and lower-laying terraces) have been delineated, both used for agriculture. The main objectives of this study were to evaluate soil chemical and geochemical properties in reclaimed zones that differ mainly in topography, soil types and agricultural land use. The origin of the trace metals in the arable soils was studied using multivariate statistics, and interpolation maps of trace metals were produced using GIS and geostatistics. Soil trace metal concentrations do not exceed a threshold value established by the Croatian Government regulation, with exception of copper. Comparative analysis of the main soil properties and trace metal concentrations in the study area showed a pronounced spatial variation and differences between two reclaimed zones in soil organic matter content, bioavailable P and total concentrations of Cd and Cu. Factor analysis in the area of the lower-laying terraces showed grouping of bioavailable P and K, organic matter content and pH (negative loading) in the component associated mostly with the land use. In the area of the fluvial terraces, bioavailable P and total Cd were grouped in the same component that may be explained by the traditional small farm agriculture and overuse of mineral fertilizers. In the whole study area, processes of secondary salinization were determined, accompanied by the raised chloride and sodium concentration measured in the saturation soil extract.     

A note on discreteness and Jevonsian deterioration in non-renewable resource exploration

Arrow and Chang's model of mineral exploration can be extended naturally to allow for deterioration in land quality, including the possibility that some land will remain unexplored even if the resource is indispensable. Discreteness is central to the necessary and sufficient conditions.     

River restoration: the fuzzy logic of repairing reaches to reverse catchment scale degradation

River restoration is an increasingly common approach utilized to reverse past degradation of freshwater ecosystems and to mitigate the anticipated damage to freshwaters from future development and resource-extraction activities. While the practice of river restoration has grown exponentially over the last several decades, there has been little empirical evaluation of whether restoration projects individually or cumulatively achieve the legally mandated goals of improving the structure and function of streams and rivers. New efforts to evaluate river restoration projects that use channel reconfiguration as a methodology for improving stream ecosystem structure and function are finding little evidence for measurable ecological improvement. While designed channels may have less-incised banks and greater sinuousity than the degraded streams they replace, these reach-scale efforts do not appear to be effectively mitigating the physical, hydrological, or chemical alterations that are responsible for the loss of sensitive taxa and the declines in water quality that typically motivate restoration efforts. Here we briefly summarize this new literature, including the collection of papers within this Invited Feature, and provide our perspective on the limitations of current restoration.     

Integrated effects of slope aspect and land use on soil nutrients in a small catchment in a hilly loess area,China

This study addressed the integrated effect of slope aspect and land use on soil nutrients in a loess hilly catchment in the western Loess Plateau of China. Soil samples were collected from five land-use types: wasteland, cropland, woodland, shrubland and abandoned cropland, at two depths (0–20 and 20–40 cm) in the middle slope position of both north-facing and south-facing slopes. Soil nutrient changes and the relationships between soil nutrients and slope aspect were investigated, based on statistical analysis and expert knowledge. Soil organic matter, total N, total P, nitrate nitrogen and available K of the 0–20 cm soil layer differed significantly between land uses and slope aspects. Soil nutrients in the north-facing slope were better than in the south-facing slope. Revegetation has an enrichment effect, especially on soil organic matter, total N, total P, nitrate nitrogen and available K. Planting of trees, shrubs and grasses could improve soil fertility and favours a policy of revegetation and sustainable land use in the hilly loess area of China. Conversion of slope farmlands into more sustainable land uses, such as shrubland or grassland is a cost-efficient way to achieve soil conservation and ecological restoration. Terracing and the use of agro-techniques for soil conservation, such as furrow-ridging tillage and leaving crop residues on fields, can increase the input of C to soils. Growing crops in rotation with alfalfa and beans could be a promising choice for the sustainability of agriculture and the environment.     

土壤学与广东持续农业的发展

持续农业是关于建立资源、生态、地力、经济效益等各个方面均可持续发展的农业制度的一种思想．水土流失、土地退化、耕地锐减、环境污染，制约着广东农业的持续发展．土壤学应围绕持续农业开展研究工作．目前应加强土壤生态环境的保护，防治土地退化，提高土壤肥力，保证耕地生产力的持续发展．应开展土壤资源的动态变化研究，为合理开发和利用土壤资源提供科学依据．