Differences among maize cultivars in the utilization of soil nitrate and the related losses of nitrate through leaching

In a 2-year field experiment conducted on a Gleyic Luvisol in Stuttgart-Hohenheim one experimental and nine commercial maize cultivars were compared for their ability to utilize soil nitrate and to reduce related losses of nitrate through leaching. Soil nitrate was monitored periodically in CaCl₂ extracts and in suction cup water. Nitrate concentrations in suction water were generally higher than in CaCl₂ extracts. Both methods revealed that all cultivars examined were able to extract nitrate down to a soil depth of at least 120 cm (1988 season) or 150 cm (1987 season). Significant differences among the cultivars existed in nitrate depletion particularly in the subsoil. At harvest, residual nitrate in the upper 150 cm of the profile ranged from 73–110 kg N ha^–1 in 1987 and from 59–119 kg N ha^–1 in 1988. Residual nitrate was closely correlated with nitrate losses by leaching because water infiltration at 120 cm soil depth started 4 weeks after harvest (1987) or immediately after harvest (1988) and continued until early summer of the following year. The calculated amount of nitrate lost by leaching was strongly influenced by the method of calculation. During the winter of 1987/88 nitrate leaching ranged from 57–84 kg N ha^–1 (suction cups) and 40–55 kg N ha^–1 (CaCl₂ extracts), respectively. The corresponding values for the winter of 1988/89 were 47–79 and 20–39 kg N ha^–1, respectively. ei]Section editor: B E Clothier     

生物淋洗修复钒污染土壤的性能与机理研究

【目的】土壤重金属污染问题日益受到关注,其中钒污染逐渐成为研究热点。淋洗是土壤修复的重要手段,但存在污染大、成本高的缺点。生物淋洗技术因其经济高效且环保的特点能够应用于土壤的修复,但其对钒污染土壤的修复,认识仍非常有限。【方法】本研究采用嗜酸性氧化亚铁硫杆菌对钒污染土壤进行了生物淋洗试验,通过影响因素试验探究了钒的最佳浸出条件,并应用扫描电子显微镜-能量色散X射线谱分析了钒在淋洗过程中的变化,最后对代谢产物进行了解析。【结果】微生物次生代谢产物能促进土壤中钒的溶出。氧化亚铁硫杆菌对土壤钒的浸出效率较高,生物淋洗20 d后土壤中钒的浸出率达到27.4%,进一步的影响因素试验表明,在固体浓度为3%、接种体积为10%、初始pH值为1.8、初始Fe²⁺的浓度为3.0 g/L的条件下,土壤中钒的浸出效果最佳。SEM-EDS分析证实生物淋洗后土壤中钒含量减少,其中以非残渣态形式存在的钒更容易被浸出。代谢组学分析显示氧化亚铁硫杆菌在浸出过程中产生了大量代谢产物来应对重金属胁迫。【结论】生物淋洗技术能够有效地实现土壤钒污染的修复,本研究为钒污染土壤提供了一种环境友好的修复方式。     

Effects of wastewater sludge and woodchip combinations on soil properties and growth of planted hardwood trees and willows on a restored site

Sludge from wastewater treatment plants and woodchips produced from urban tree pruning residues were used to improve soil conditions of a degraded site restored by planting trees and shrubs. The release of soil nitrogen resources was set by the proportions of sludge and woodchips applied. Combining 187 kg N/ha of sludge in one application with 200 m³/ha of woodchips instead of 100 m³/ha reduced first year N mineralization by 50%. The same can be said for the application of 125 kg N/ha of sludge in two applications, over 2 years. The degradation of sludge–woodchips and nitrate leaching was reduced even with the smallest sludge application. Survival and growth of Acer saccharinum L., Fraxinus pennsylvanica Marsh. and Salix discolor Muhl. did not vary much with sludge and woodchips quantities. However, differential soil nitrogen availability and the degradation process of organic amendments induced by the treatments may result in better sustainable growth for planted woody species. Some undesirable elements were measured in the soil, particularly Fe, Cd, Pb and NO₃–N. Because of these, care should be taken when choosing sites to be restored using sludge and woodchips.     

Target regions for silvoarable agroforestry in Europe

Silvoarable agroforestry (SAF) has recently been proposed as an alternative land-use system for Europe. Data on soil, climate, topography, and land cover were integrated in a geographic information system (GIS) to identify agroforestry target regions where (i) productive growth of trees (Juglans spp., Prunus avium, Populus spp., Pinus pinea, and Quercus ilex) in SAF systems could be expected and where (ii) SAF systems could potentially reduce the risk of soil erosion, nitrate leaching and increase landscape diversity.The analysis shows that the investigated tree species could grow productively in SAF systems on 56% of the arable land throughout Europe (potential productive tree growth area). 80% of the European arable land was classified as potential risk area for soil erosion, nitrate leaching, and/or landscape diversity. Overlaying potential productive tree growth areas with the arable land that was considered as environmental risk area yielded target regions. They were found to make up about 40% of the European arable land and thus SAF could contribute to soil protection on 4%, to mitigate nitrate leaching on 18% and to increase landscape diversity on 32% of European arable land.Although limited by constrained data availability, the study shows that SAF could be implemented in a productive way throughout Europe and that it could help resolve some of the major land-use problems. The environmental benefits could justify the support of SAF by subsidies.     

不同土地利用方式土壤氨氧化微生物和反硝化微生物时空分布特征

研究不同土地利用方式下氮循环相关微生物在不同土壤剖面的分布,可为认识和理解土壤氮转化过程提供科学依据。土壤氨氧化微生物和反硝化微生物在调节氮肥利用率、硝态氮淋溶和氧化亚氮(N₂O)排放等方面有着重要作用。以北京郊区农田和林地两种土地利用方式为研究对象,分析土壤氨氧化潜势和亚硝酸盐氧化潜势在0—100 cm土壤剖面上的季节分布(春季和秋季),并通过实时荧光定量PCR方法表征土壤氨氧化和反硝化微生物的时空分布特征。结果表明,农田土壤氨氧化潜势、亚硝酸盐氧化潜势、氨氧化微生物和反硝化微生物丰度均显著高于林地土壤,且随土壤深度增加而显著降低。除氨氧化古菌amoA基因丰度在不同季节间无显著差异外,春季土壤氨氧化细菌(amoA基因)、反硝化微生物nirS、nirK和典型nosZ I基因的丰度均显著高于秋季。土壤有机质、总氮、NH~+₄-N、NO~-₃-N含量与氨氧化微生物和反硝化微生物的功能基因丰度显著相关。综上,不同土地利用方式下土壤氮循环相关微生物的丰度与土壤氮素的可利用性和转化过程紧密相关,研究结果对土壤氮素利用和养分管理提供...     

氮磷添加对草甸草原土壤氮磷转化功能基因丰度的影响

氮添加是提高退化草地生产力的主要养分管理措施,而过量的氮输入会导致土壤酸化、增加硝酸盐淋溶损失和温室气体排放。旨在明确草原割草利用下土壤氮、磷转化功能基因丰度对氮磷添加的响应规律,为定向调控打草场土壤氮、磷转化过程,提高养分利用效率,减少温室气体N₂O排放提供科学依据。2018—2020年在呼伦贝尔草甸草原打草场设置了5个施氮水平(0、1.55、4.65、13.95、27.9 g N m^-2 a^-1)和3个磷水平(0、5.24、10.48 g P m^-2 a^-1),裂区试验设计,在植物不同生长时期测定土壤氨氧化(amoA-AOA和amoA-AOB)、反硝化(narG、nirK、nirS和nosZ)和磷转化(phoD)基因丰度。结果表明,土壤氮转化基因丰度受到氮、磷添加的调控,而氮、磷添加对土壤磷转化功能基因丰度无显著影响(P>0.05)。氮添加可提高amoA-AOB基因丰度,增加氨氧化细菌调控土壤总硝化速率的相对重要性,因此能增加硝酸盐淋溶损失潜势。高氮处理下添加磷可降低...     

Heterotrophic nitrification in a health soil demonstrated by anin situ method

Summary Nitrate reductase activity (NRA) in the leaves of two subspecies ofHypochaeris radicata was taken as a parameter for nitrate production in the soilin situ. Ammonium addition to the soil ofH. radicata ssp.radicata (soil pH 6.2) resulted in an increase of NRA, thus indicating nitrate formation by chemolithotrophic nitrifiers after a certain time-lag. Addition of ammonium to the soil ofH. radicata ssp.ericetorum (soil pH 4.3) dit not affect NRA in the leaves. Tests based on the MPN method failed to demonstrate the occurrence of chemolithotrophic nitrifiers in this soil. However, the addition of peptone led to an increase of NRA within seven days, which indicates the presence of heterotrophic nitrifying organisms. The results obtainedin situ were confirmed in a laboratory experiment, where soil samples were incubated in the presence and absence of (NH₄)₂SO₄ or peptone. The addition of ammonium led to a decrease in the production of nitrate to zero as compared with the control in the acid soil of ssp.ericetorum, whereas the addition of peptone resulted in nitrate levels amounting to about twice the control value. In the soil of ssp.radicata nitrate formation showed a rapid increase, compared with the control, after the addition of ammonium as well as after the addition of peptone.Grassland species research group, publication no27     

复合菌剂调控连作当归根围土壤养分及对产量的影响

【背景】连作可引起微生物群落结构失调,导致土壤环境恶化、养分循环不畅、当归[Angelica sinensis (Oliv.) Diels]产量降低,通过现代微生物技术改良土壤、消减连作障碍势在必行。【目的】于大田条件下,研究施用复合菌剂对当归根围土壤酶活、速效养分及产量的影响,明确增产机制,改进增产措施。【方法】利用溶磷圈法检测不同菌株溶磷活性、乙炔还原法检测固氮活性、试剂盒法检测过氧化物酶和硝化能力;复合菌剂T1[荧光假单胞菌(Pseudomonas fluorescens)CBS5、产碱假单胞菌(Pseudomonas alcaligenes) CBS7、嗜冷假单胞菌(Pseudomonas extremaustralis)CBSB、生枝动胶菌(Zoogloea ramigera) CBS4]和T2 (荧光假单胞菌CBS5、产碱假单胞菌CBS7、嗜冷假单胞菌CBSB)及对照CK (无菌马铃薯葡萄糖肉汤培养基)分别处理连作当归,分光光度法测定根围土壤及根中养分循环、转化相关酶活,氮、磷、钾速效养分含量;常规方法测产量;统计软件进行相关数据方差分析和主成分分析。【结果】产碱假单胞菌C...     

基于秸秆还田条件下的黄灌区稻旱轮作土壤硝态氮淋失特征研究

宁夏引黄灌区农田面源污染较为严重,区内大部分排水沟水质为劣Ⅴ类,其主要污染物硝态氮与铵态氮。设置常规施肥(CK)、常规施肥条件下施用4500kg/hm~2(T1,半量还田)和9000 kg/hm~2(T2,全量还田)秸秆3个处理。利用树脂芯法吸附10、20、30、60、90cm土层的硝态氮流失量。2009—2013年的试验结果表明:秸秆还田能够减少土壤30cm土层的硝态氮淋失。与对照硝态氮淋失量(15.76 kg/hm~2)相比,T1(13.76 kg/hm~2)与T2(13.74 kg/hm~2)均达到显著差异(P0.05),淋失量分别减少12.71%和12.84%,T1与T2没有达到显著差异。秸秆还田对土壤硝态氮淋失的影响效应主要体现在30cm土层处,10、20、60与90cm土层处的处理与对照都没有达到显著差异。秸秆还田提高了30cm土层的土壤有机质与土壤总氮,与对照(13.78 g/kg)相比,T1与T2土壤有机质分别提高0.89 g/kg和1.24 g/kg;试验结束后,对照、T1和T2的总氮是达到0.64、0.66和0.69 g/kg,与对照相比,处理分别提高了2.76%和6.83%。秸秆还田有助于作物增产,T1与T2的水稻平均增产9.24%和10.37%,小麦增产10.11%和11.51%。     

3种菊科入侵植物不同生长时期的土壤酶活性和养分变化

【目的】黄顶菊、三叶鬼针草和豚草是我国危害较严重的3种菊科入侵植物。了解3种菊科植物生长过程中土壤养分和酶活性的变化,可以为研究其入侵机制提供依据。【方法】在中国农业科学院植物保护研究所廊坊中试基地开展同质园实验,比较分析了黄顶菊、三叶鬼针草和豚草3种菊科入侵植物在幼苗期、旺盛生长期和生殖生长期根际土壤养分和酶活性的变化。【结果】3种外来菊科植物的生长时期对土壤养分和酶活性存在显著影响。3种外来植物入侵域的土壤速效磷、硝态氮含量以及磷酸酶活性随生长时期变化都表现出先升高后降低的趋势,均在旺盛生长期达到最大值。入侵域土壤速效磷和硝态氮含量的变化趋势与狗尾草明显不同。3种外来植物入侵降低了土壤速效钾含量,提高了土壤脲酶、磷酸酶活性。【结论】3种外来菊科植物的入侵改变了土壤养分和酶活性,创造出更有利于自身生长和繁殖的条件,以利于其进一步扩张。     

Drainage and nitrate leaching in a crop rotation under different N-fertilizer strategies: application of capacitance probes

Quantification of drainage and nitrate leaching from cropping systems is necessary to optimize N-fertilizer application and determine the impact on groundwater quality. The objectives of this work were to (i) assess the use of capacitance probes for the continuous determination of the volume of drainage water and the amount of nitrate leached in a crop production system, and (ii) compare the effect of different N-fertilizer strategies to control nitrate leaching in a crop rotation in humid Mediterranean climate. A factorial (control and three fertilizer strategies) experiment was conducted during three cropping seasons in Navarra (Spain). Wheat (Triticum aestivum L.) was planted in 2002, barley (Hordeum vulgare L.) in 2003, and rapeseed (Brassica napus L.) in 2004. Daily soil water content measurements based on capacitance probes were used to calculate drainage at 1 m depth, by applying the water balance equation. Nitrate leaching was calculated as the drainage volume multiplied by the nitrate concentration of the soil solution extracted in ceramic cups. The results revealed distinct behaviour in three crop phases, viz.: (i) from planting to GS-25, with high risk of drainage and nitrate leaching, (ii) from GS-25 to the end of the drainage period, with little drainage and leaching, and (iii) from then to harvest, when no drainage or nitrate leaching took place. Drainage and soil mineral N content before planting were the main factors determining the amount of N leached. Splitting N-fertilizer application and the use of nitrification inhibitors are not likely to have a significant impact on subsequent N-leaching losses, provided that the N-fertilizer application is adjusted to crop N needs corrected by soil N supply.     

Hydrologic flowpaths influence inorganic and organic nutrient leaching in a forest soil

Hydrologic pathways through soil affect element leaching by determining the relative importance of biogeochemical processes such as sorption and decomposition. We used stable hydrogen isotopes of water (δD) to examine the influence of flowpaths on soil solution chemistry in a mature spruce–hemlock forest in coastal Oregon, USA. Soil solutions (50 cm depth, n = 13) were collected monthly for 1 year and analyzed for δD, major ions and dissolved organic carbon (DOC) and nitrogen (DON). We propose that the variability of δD can be used as an index of flowpath length and contact time. Throughfall variability in δD was much greater than soil solution variability, illustrating that soil solution integrates the variation in inputs. Lysimeters with greater variation in δD presumably have a greater proportion of flow through rapid flowpaths such as macropores. The variation in soil solution δD for individual lysimeters explained up to 53% of the variation in soil solution chemistry, and suggests that flowpaths influence leaching of some constituents. Soil solutions from lysimeters with greater δD variation had higher DOC and DON (r ² = 0.51 and 0.37, respectively), perhaps because transport via macropores reduces interaction of DOM with the soil matrix. In contrast, nitrate concentrations were highest in lysimeters with a small variation in δD, where long contact time and low DOC concentrations may yield higher net nitrification. Our results demonstrate the utility of stable isotopes to link flowpaths and soil solution chemistry, and illustrate how the spatial complexity of soils can influence ecosystem-level nutrient losses.     

Nitrate leaching from three afforestation chronosequences on former arable land in Denmark

In regions dominated by agricultural activities, nitrogen (N) is recognized as a major pollutant in aquatic environments. In north‐western Europe, afforestation of agricultural land is part of a strategy to improve water quality. In Denmark, former arable land has been afforested during the past 40–50 years. This study evaluated the effect of afforestation of former arable land on nitrate leaching, based on three afforestation chronosequences. Precipitation, canopy throughfall and soil water were collected and soil moisture was monitored at two Danish locations, Vestskoven (nutrient‐rich, medium deposition) and Gejlvang (nutrient‐poor, high deposition). Afforestation was performed using Norway spruce [Picea abies (Karst.) L.] and common oak (Quercus robur L.) at Vestskoven and Norway spruce at Gejlvang. The results suggest that afforestation of former arable land initially leads to lower nitrate leaching than that occurring under the former agricultural land use, and largely below the standard of 50 mg NO⁻₃ L⁻¹ for groundwater to be utilized as drinking water. Nitrate concentrations became almost negligible in forest stands of 5–20 years of age. However, after canopy closure (>20 years) nitrate concentrations below the root zone and nitrate leaching tended to increase. This was attributed to increased N deposition with increasing canopy development and decreased N demand once the most N‐rich biomass compartments had been built up. Nitrate leaching started to increase at a throughfall deposition level of about 10 kg N ha⁻¹ yr⁻¹. Compared with nutrient‐poor sandy soils, nutrient‐rich clayey soils appeared more vulnerable to disturbance of the N cycle and to increased N deposition, leading to N saturation and enhanced nitrate leaching. In approximately the first 35 years after afforestation, nitrate leaching below the root zone was generally higher below oak than below Norway spruce.     

氮添加对贝加尔针茅草原土壤线虫群落特征的影响

以内蒙古贝加尔针茅草原为研究对象,通过氮素添加(0、15、30、50、100、150、200、300 kg N hm~(-2)a~(-1))模拟氮沉降的控制实验,研究氮沉降对内蒙古贝加尔针茅草原土壤线虫的群落结构和多样性的影响。结果表明,在本实验所有样品中共鉴定出52个属,优势类群为螺旋属(Helicotylenchus)、丽突属(Acrobeles)和真滑刃属(Aphelenchus)。土壤线虫具有明显的表聚现象,相对密度变化不显著。从功能类群上看,随着氮素添加水平的增加,食细菌类群(Bacterivores)线虫和捕食类群/杂食类群(Predators/Omnivores)线虫氮素添加水平均成负相关。从生态指标来看,在N50施氮范围内对土壤线虫的丰富度(SR)、多样性(H')、均匀度(J')等生态指标有促进作用;通路指数在试验的所有处理中都小于0.75,表明土壤中的有机质分解途径是以真菌为主;瓦斯乐思卡指数表明,少量施氮可以改善土壤的环境状况,减少植物寄生类群(Plant parasites)线虫对植物群落及生产力的影响。当施氮量N100时,土壤pH值显著降低,硝态氮和铵态氮显著增加,土壤中生活史k对策者的线虫显著减少,r对策者显著增加,世代交替加快,土壤线虫群落结构显著变化。     

Alleviation of salt-induced stress on seed emergence using soil additives in a greenhouse

Use of sodium chloride (NaCl) as a deicing salt results in high concentrations of ions in roadside soils, which decreases seedling emergence in these areas. Greenhouse experiments performed in soil culture tested the efficacy of three soil fertilizers, gypsum (CaSO₄), potash (potassium chloride, KCl) and potassium nitrate (KNO₃), in alleviating NaCl stress on seedling emergence of three grass species exhibiting a range of salt tolerance, Poa pratensis (Kentucky bluegrass), Bouteloua gracilis (blue grama), and Puccinellia distans (alkali grass). Two-factor factorial designs were utilized for each species-fertilizer combination. Treatments of 5000 mg/L (0.086 M) NaCl with or without fertilizer, in concentrations that were equal to 0.5, 1, and 2 times the molar equivalent of 5000 mg/L NaCl were applied biweekly. Salt stress on Poa pratensis emergence was alleviated by all fertilizers with CaSO₄ having the greatest effect in alleviating NaCl stress and potash and potassium nitrate alleviating stress at lower treatment levels. Emergence of Bouteloua gracilis and Puccinellia distans was in most cases negatively effected by soil amendments.     

闽江河口春季互花米草入侵过程对短叶茳芏沼泽土壤碳氮分布特征的影响

2014年4月,选择闽江口鳝鱼滩湿地中未被入侵的短叶茳芏群落(A)、互花米草入侵斑块边缘(B)以及互花米草入侵斑块中央(C)为研究对象,基于时空互代研究方法,探讨了互花米草入侵序列下湿地土壤碳氮空间分布特征的差异。结果表明,互花米草入侵显著降低了土壤的NO_3~--N含量(P0.05),但整体增加了NH_4~+-N含量,这与其入侵后导致湿地土壤颗粒组成发生显著变化(砂砾含量增加33.81%),进而促进了土壤的矿化作用和硝化作用,并有助于硝态氮的垂直淋失有关。互花米草入侵整体增加了土壤的碳氮含量和C/N比,与入侵进程和入侵前相比,互花米草入侵后湿地土壤的碳储量分别增加了8.73%和24.37%,氮储量则分别增加了10.22%和17.87%,这主要与其对闽江口湿地植物群落格局、养分生物循环以及强促淤作用引起的土壤颗粒组成等显著改变有关。研究发现,闽江口互花米草入侵对短叶茳芏湿地土壤碳氮含量的影响相对于江苏盐城、长江口以及杭州湾湿地的影响可能更为显著,其互花米草入侵较大改变了土壤中陆源和海源有机质的来源比例,使得入侵后湿地土壤养分的自源性增强。     

Seasonal distribution of topsoil ammonium and nitrate under legume-grass and grass swards

Losses of soil N through leaching and N₂ fixation by legumes often are related to soil nitrate concentration. The seasonal distribution of soil ammonium and nitrate concentrations under ungrazed legume-grass and grass swards were evaluated on two experiments that were established in 1983 (Exp. 1) and in 1984 (Exp. 2). Treatments were white clover (Trifolium repens L.) (WC), red clover (Trifolium pratense L.) (RC), and birdsfoot trefoil (Lotus corniculatus L.) (BT), each grown with tall fescue (Festuca arundicacea Schreb.) (TF) at two legume proportions, and a pure stand of TF. The concentrations of both forms of N were measured in the top 20-cm layer during 2 years in Exp. 1 and for 1 year in Exp. 2. The concentrations of nitrate and ammonium were least in winter and spring, and greatest in summer. The concentration of nitrate for the mixtures decreased in the order WC-TF, RC-TF, and BT-TF in both summers of Exp. 1 but there were no mixture differences in Exp. 2. The concentration of soil ammonium was not affected by the treatments applied. We conclude that the concentration of soil nitrate usually was small for these swards but became greater and often dependent on species and legume proportion during summer. The concentration of soil ammonium also was greater in summer but was not affected by species or legume proportion. Journal of Paper no. J.-13359 of the Iowa Agric. and Home Econ. Exp Stn., Ames. Project 2281. Supported in part by the Facultad de Agronomía, Montevideo, Uruguay. Journal of Paper no. J.-13359 of the Iowa Agric. and Home Econ. Exp Stn., Ames. Project 2281. Supported in part by the Facultad de Agronomía, Montevideo, Uruguay.     

Evaluation of laboratory-based measures of soil mineral nitrogen and potentially mineralizable nitrogen as predictors of field-based indices of soil nitrogen supply in potato production

Accurate estimation of soil nitrogen (N) supply in the field is required to optimize fertilizer N management and to minimize environmental N losses in humid environments. Laboratory-based measures of N availability were evaluated as predictors of field-based indices of soil N supply within potato production systems. Pre-plant soil samples (0–15 cm) were collected from a series of forty treatments in established potato trials located in Atlantic Canada and Maine, USA. Total plant N uptake at topkill with no fertilizer N applied (PNU_0N), PNU_0N plus soil mineral N to 30 cm depth at harvest and relative yield were considered as field-based indices of soil N supply. The potentially mineralizable N (N₀) was determined by aerobic incubation at 25°C and periodic leaching for 24 weeks. A series of laboratory-based measures of soil N supply were measured in soil samples. Pre-plant soil nitrate or total mineral N at 0–30 cm depth was the best single predictor of PNU_0N (r = 0.67 and 0.71, respectively) and relative yield (r = 0.58 and 0.61). The ultraviolet absorbance of 0.01 M NaHCO₃ extract at 205 nm (NaHCO₃-205) was suitable as a predictor of PNU_0N and relative yield in each growing season, however, the relationship between this parameter and PNU_0N or relative yield varied somewhat among years. A combination of pre-plant mineral N plus N mineralized in the first 2 weeks period of incubation after re-wetting is proposed as a more robust measure of N availability compared with use of mineral N alone.     

Assessing nitrate leaching during the three‐first years of Miscanthus × giganteus from on‐farm measurements and modeling

Miscanthus × giganteus is often regarded as one of the most promising crops to produce sustainable bioenergy. This perennial crop, renowned for its high productivity associated with low input requirements, in particular regarding fertilizers, is thought to have low environmental impacts, but few data are available to confirm this. Our study aimed at assessing nitrate leaching from Miscanthus × giganteus crops in farmers' fields, thus including a wide range of soil and cropping system conditions. We focused on the first years of growth after planting as experimental studies have suggested that Miscanthus × giganteus, once established, results in low nitrate leaching. We combined on‐farm measurements and modeling to estimate drainage, leached nitrogen, and nitrate concentration in drainage water in 38 fields located in Center‐East France during two winters (November 2010 to March 2011, November 2011 to March 2012). Nitrate leaching and nitrate concentration in drainage water were on average very low. Nitrate leaching averaged 6 kg N ha^?1 whereas nitrate concentration averaged 12 mg l^?1. These low values are attributable to the low estimates of drainage water (mean = 166 mm) but also to the low soil mineral nitrogen contents measured at the beginning of winter (mean = 37 kg N ha^?1). Our results were, however, very variable, mainly due to the crop age: nitrate leaching and nitrate concentration were critically higher during the winter following the first growth year of Miscanthus × giganteus, reflecting the low development of the crop. This variability was also explained by the range of soil and cropping conditions explored in the on‐farm design: shallow and/or sandy soils as well as fields where establishment failed had a higher risk of nitrate leaching.     

Isopod effects on decomposition of litter produced under elevated CO2, N deposition and different soil types

The performance of Oniscus asellus (Isopoda) and its influence on litter mass loss and mineralization was assessed in a microcosm experiment, using beech (Fagus sylvatica) leaf litter that was produced on different soil types, contrasting atmospheric CO₂ concentrations, and different nitrogen deposition rates. Litter quality was significantly altered by these treatments, and many of the CO₂ and N effects differed between soil types. Litter quality affected subsequent litter mass loss rates, microbial respiration, and leaching of dissolved organic carbon (DOC) and nitrate. These effects were largely independent of the presence of isopods, even though isopods highly accelerated litter mass loss, stimulated microbial respiration by 37%, and increased nitrate leaching by 50%. Isopods did not change their relative rates of litter consumption and growth in response to litter quality. Isopod mortality, however, increased with increasing litter lignin/N ratios, and was significantly different between soil types, which may indicate long‐term effects on litter decomposition through altered isopod densities. Having the choice among the litter of three different species [maple (Acer pseudoplatanus), beech (Fagus sylvatica) and oak (Quercus robur)] grown at either ambient or elevated CO₂, isopods preferred maple to beech when all the litter was produced under elevated CO₂. This suggests that beyond changes in consumption, an altered food selection by isopods in a CO₂‐enriched atmosphere may affect the temporal and spatial composition of the litter layer in temperate forests. In contrast to previous findings, we conclude that isopods do not always increase their consumption rates, and hence do not differentially affect microbial decomposition in litter of poorer quality. Nevertheless changes in animal densities and/or shifts in their food preferences, could result in altered decomposition and carbon and nutrient turnover rates.