Untersuchungen zur Stickstoff-Immobilisation in mineralisch gedüngten Ackerböden aus Löß während der Vegetationszeit von Winter-Weizen

Experiments on nitrogen immobilization in minerally fertilized soils from loess during the growing season of winter wheat The nitrogen regime has been simulated during the growing period of winter wheat 1984/85 on a stagnigleyic cambisol using a simple, functional computer model. The model includes N mineralization from soil organic matter, transport of water and nitrate as well as growth of wheat and N uptake by the crop. Simulation starts at harvest of the previous crop. Simulated and measured N supply (soil mineral nitrogen plus N uptake by the plant) were in good agreement between september and december 1984. On this loess plot as well as on 10 other ones an over-estimation of mineral nitrogen in the soil up to 40 kg/ha was observed with beginning of december/january 1984/85 reflecting a seasonal trend. Experiments with ¹⁵N enriched Ca-nitrate 1984/85 on microplots of the same field point to a non-consideration of nitrogen immobilization. Fertilizer-N-immobilization amounted up to 35 kg/ha in the soil and to further 15 kg/ha in the straw material. The pool of fixed ammonium was of no importance with respect to the mobilization-immobilization-turn-over of fertilizer nitrogen. Experiments 1988/89 on microplots of a colluvial loess soil indicate a change of biomass nitrogen being responsible for the seasonal N-immobilization. An increase of biomass-N of about 30 kg/ha was observed under the growing wheat crop. An additional N-immobilization of nearly 40 kg/ha was observed with straw incorporation. A similar increase of microbial biomass nitrogen under winter wheat has been observed during the growing period 1987/88.     

Kali-Düngeempfehlung auf der Grundlage von 81 K-Düngungsversuchen zu Getreide und Zuckerrüben auf Lößböden in Südniedersachsen

K-fertilization recommendation on the foundation of 81 experiments with small grains and sugar beets on ‘loes’soils in the southern part of Lower Saxony (West Germany) In no case was it possible to increase the grain yield of winter wheat and winter barley with K-fertilization. However, in the average of 24 experiments with sugar beets, K-fertilization increased significantly the sugar yield. The amount of K-fertilization necessary for sugar beets on the single fields could not be determined by the K soil analysis. Based on these results, which were received mainly on deep rootable and many years intensively fertilized ‘loess’soils, the following K-fertilization for a crop rotation of sugar beets and 2 × small grain is recommended: Independent of the K-content of soils for sugar beets 200 kg K₂O/ha should be applied if the crop residues remain on the field. However, for small grains a mineral K-fertilization is not necessary. If the residues are not returned to the soil the amount of K contained in the residues must be additionally applied.     

Quantitative und qualitative Veränderungen im A-Horizont von Sandböden nach Umwandlung von Dauergrünland in Ackerland

Quantitative and qualitative changes in soil properties of A- horizons of sandy soils caused by conversion of grassland to arable land Changes in physical soil properties and in soil organic matter of the A-horizons due to the conversion of permanent grassland to arable land are quantified and described as a function of time for sandy soils. The study was carried out in an area northeast of Hannover. A decrease of about 100 t/ha C_org (- 57%), 5 – 6 t/ha N_org (- 58%) and 1 t/ha S_t (- 58%) was measured for a period of 2 – 4 years after grassland conversion. Thereby the quality of the soil organic matter remains unchanged (no changes of the C/N ratio and of the distribution of N_org in 5 N-fractions). However, an increase of soil bulk density from 1.0 to 1.3 g/cm³ and a decrease of total pore volume from 0.59 to 0.47 were observed. The fast mineralization of soil organic matter in the A-horizon following the conversion of grassland soils results in a temporary heavily increased nitrate input into the groundwater. Furthermore mineralization and leaching of nitrate and sulfate induces an acidification push in the soil by a proton release in the order of 350 keq/ha during a 2 – 4 years period. However, this proton production is compensated quantitatively by several applications of lime or marl by farmers and by the buffering of bases cations released from mineralized soil organic matter.     

The Static Fertilization Experiment at the Start and the End of the 20th Century

Changes of yields, nitrogen uptake on the zero plots and nitrogen balances are discussed in the course of the decades at the Static Fertilization Experiment exemplary. 1991-2000 yields of cereals on the fertilized plots were nearly 200% in comparison to 1906-1915. At potatoes and sugar beets increase of yields was smaller. In the middle of all crops 52kg/ha nitrogen were taken up on the unfertilized plots in the years 1959-2000. Since there is a balance in the soil this nitrogen can only derived from the air. On the PK plots the atmogenic nitrogen input is 6kg/ha still higher. Crops with a long vegetation period like winter wheat and sugar beets take up more atmogenic nitrogen than such with a shorter vegetation period like summer barley and potatoes. The atmogenic nitrogen input per day of vegetation period is between 0,24 (winter wheat) and 0,38 (sugar beet)kg/ha and day. Nitrogen balances of the more important variants show that nitrogen uptake is higher than nitrogen input for a long time. In comparison of the decades 1961-1970 and 1991-2000 the best effect is in the case of mineral fertilization alone, also at increasing nitrogen input at the end of the century. The reason is the optimal control of nitrogen amount and time of application. In contrast organic fertilization and nitrogen release from the organic matter you can't control with the result of more unfavourable balances.     

Nmin−Gehalt im Boden,mineralische N-Düngung und N-Entzug von Winterweizen im Internationalen Organischen Stickstoffdauerdüngungsversuch (IOSDV) Berlin-Dahlem

N_mim content in the soil, N-fertilization and N uptake of winter wheat in the international organic nitrogen long-term fertilization experiment (IOSDV) Berlin-Dahlem During the 9th and 10th year of the long-term IOSDV field experiment micro plots were put in three treatments. Labelled¹⁵ N (160 resp. 110 kg/ha N as ammonium sulfate) was fertilized to winter wheat subdivided into three portions. N_min in soil was determined five times during the season, plant biomass was harvested at different growth stages and N uptake was calculated. Using the¹⁵ N-technique permitted a discrimination between fertilizer-N and soil-N. Preferential uptake of fertilizer-N by the wheat crop but also immobilisation in soil were observed until June. Subsequently the immobilized N was remineralized and assimilated by wheat. But the native N_min of soil was minimaly utilized during the initial growth of wheat. Therefore the absolute amount of soluble N temporarily increased caused by a mineralisation of the organic matter.     

Simulation of nitrogen dynamics in farmland areas of Denmark (1989–1993)

Abstract. Each year since 1986 information has been collected about the farming systems at intersections of a nationwide 7 km square grid in Denmark. These management data and corresponding soil analyses were used in the model DAISY to simulate water and nitrogen dynamics. The model was validated with respect to harvested dry matter yield and nitrogen content in the soil. Simulated nitrate leaching from farmland areas from 1 April 1989 to 31 March 1993 was related to precipitation zones, soil type, fertilizer strategies and cropping systems. The mean simulated nitrate leaching for the whole of Denmark was 74 kg N/ha/yr, with a large yearly variation in the period considered. The simulated nitrate leached from soils with a sandy subsoil corresponded to 51% of the applied fertilizer, twice that leached from soils with a loamy subsoil. The application of pig manure resulted in average leaching losses of 105 kg N/ha/yr. The simulated nitrate leaching losses at sites where only artificial fertilizer was applied were in the following order: cereal with undersown grass < crop followed by winter cereal or winter rape < cereal or rape without a catch crop < root crops without a catch crop. Where only artificial fertilizers were applied, the simulated mean annual leaching was 59 kg N/ha from spring barley and 40 kg N/ha from winter wheat. A map of simulated nitrate leaching in Denmark was produced using a Geographical Information System.     

潮土区29年来土壤肥力和作物产量演变特征

【目的】 潮土是我国重要的农业土壤,是小麦和玉米的主产区。本研究对29年来全国潮土长期定位试验监测的数据进行了分析,明确了潮土区土壤养分状况、肥力水平以及产量变化特征,为潮土区的养分管理和合理施肥提供科学依据。 【方法】 基于分布在我国12个省、市、自治区的51个潮土肥力长期监测基地,整理分析了潮土29年来5个肥力指标 (有机质、全氮、有效磷、速效钾、pH) 以及作物产量随监测年限的变化。监测期10～29年,监测区种植的作物主要为小麦和玉米,种植方式包括小麦?玉米、冬小麦?夏玉米、春小麦?夏玉米轮作。本研究将监测时间分为监测初期 (1988—1997年)、监测中期 (1998—2003年) 和监测后期 (2004—2016年) 三个阶段,并进行了三个监测时期各肥力指标和产量平均值的比较,运用主成分分析法分析了土壤综合肥力的主要贡献因子。 【结果】 潮土有机质、全氮、有效磷、速效钾含量整体呈上升趋势,而pH呈下降趋势。土壤有机质和全氮从监测初期到监测中期分别显著提升了47.1%、37.8%,中期到后期提升未达到显著水平;土壤有效磷从监测初期到监测后期逐步提升226%,监测初期与后期差异显著;土壤速效钾从监测初期到中期略有下降,监测中期到后期显著提升了30.4%;土壤pH呈下降趋势,尤其从监测中期的8.14到监测后期的7.78;潮土区常规施肥下小麦和玉米产量的变化随时间呈现出明显上升的趋势,监测中期小麦的平均产量比监测初期显著增加了87.6%,监测中期与后期产量差异不显著;玉米的平均产量从监测初期到监测中期显著提升了111%。主成分分析结果表明,潮土区土壤全氮和有机质是潮土综合肥力的主要影响因素。 【结论】 经过10～29年的常规施肥,潮土区土壤的单一肥力、综合肥力以及作物产量先后都得到了显著提高,虽然pH有明显降低。土壤综合肥力和作物产量的变化主要取决于土壤全氮和有机质含量,因此,施肥过程中要适当控制氮肥的比例和用量。      

Prüfung der Nachwirkung organischer Düngungsstufen eines Stickstoffdauerdüngungsversuches (IOSDV/Oldenburg) im Gefäßversuch: (The after effect of long term different organic fertilisation of a permanent nitrogen fertiliser field experiment in a pot experiment)

Abstract

After nine experimental years in a field trial with four fertiliser treatments combined with five mineral N treatments and cultivation of sugar beets, winter wheat and winter barley yearly the after effect has been tested in a pot experiment with raygras. After the end of the field trial soil has been taken from all the four organic treatments, from two mineral N treatments and from each crop in the crop rotation. The after effect of nine years different organic fertilisation has been proved to be apparent, but is heavily covered by the effect of the precrop and partly also by the N-fertilisation in the field. Nevertheless the second organic fertiliser treatment (catch crop, straw, leaves of sugar beets) was concerning the after effect more effective compared with the treatment application of pig slurry yearly to all crops or the application of pig slurry once in three years to sugar beets.The effect of the last cultivated crop in the field trial influenced the after effect of grass in some cases significantly. Sugar beets were superior to winter wheat and winter barley.The N-contents in the grass and the N-uptake were significantly influenced by the additional N-application in the pot experiment. The other factors were only of small influence.Summarizing the results of the pot trial show, that after nine years different organic fertilisation no clear evaluation is possible about its after effect, due to partly significant interactions with the precrop and the mineral N-fertilisation.     

Phosphat-Düngerbedarf von Getreide und Zuckerrüben im südniedersächsischen Lößgebiet

Phosphate fertilizer requirement of cereals and sugar beets on “loess soils” in the Southern part of Lower Saxony (F.R. of Germany) In the years 1984 to 1986 105 P-fertilizer experiments with winter wheat, winter barley and sugar beets were carried out on “loess soils” in the Southern part of Lower Saxony (F. R. of Germany). The mineral P fertilization applied as “Triplephosphat” varied between 0 and 250 kg P₂O₅/ha. Soil test values (P-H₂O method) of the sites ranged from 6 to 38 and were on the average 18 ± 8 mg P/kg. Besides the P-H₂O-extraction the following methods were used: CAL, DL, NaHCO₃ and EUF. In no case P-application increased yields of cereals and sugar beets, although in 1986 there was no P fertilization for three years. Results of plant analysis (0.3–0.6% P i. dm) also showed a sufficient P-status. Furthermore an increase of P content of soils (+20 mg P-H₂O/kg on average) by a fertilizer rate of 1500 kg P₂O₅/ha did not effect yield in the following years. Thus, on these fields with P levels of 5 mg P-H₂/kg soil (5 mg P₂O₅-CAL/100 g) and more a P fertilization corresponding to the P removal by the crop rotation of sugar beets and 2x cereals of about 180 kg P₂O₅/ha in three years is recommended, if crop residues remain on the field. At P levels higher than 12–14 mg P-H₂O/kg soil P fertilization can be below P-removal or omitted.     

有机无机肥配施提高旱地麦田土壤养分有效性及酶活性

【目的】有机无机肥配施可显著提高土壤微生物活性,改善土壤养分供应状况。深入理解不同氮肥用量配施有机肥下土壤的生物化学性状,为充分发挥肥料效益,实现冬小麦高产稳产提供科学施肥依据。【方法】以冬小麦为供试作物,在黄土高原南部半湿润易旱区连续三年进行了田间定位试验。采用裂区试验,设置5个氮肥用量 (N 0、75、150、225、300 kg/hm2),配施或不施有机肥 (30 t/hm2)。在冬小麦拔节期、抽穗期、灌浆期、成熟期,取0—20 cm土层样品,采用常规方法测定土壤养分和酶活性。在收获期,调查了冬小麦籽粒产量。【结果】1) 冬小麦产量以施氮量N 150 kg/hm2配施有机肥处理最高,且有机无机肥配施与单施化肥处理相比能够在减少19.1%的氮肥用量条件下,保证冬小麦产量稳产高产,此外在天气不理想的状况下,冬小麦的净收益也能保持在较高水平。2)在冬小麦的整个生育期,有机无机肥配施处理可显著提高0—20 cm土层土壤有机质、全氮、有效磷、速效钾、硝态氮含量以及土壤蔗糖酶、碱性磷酸酶和脲酶活性,与单施化肥处理相比分别增加18.2%、27.4%、149.3%、31.4%、27.6%、4.0%、4.7%、1.5%,但对过氧化氢酶活性无明显促进作用,且除了脲酶以施氮量N 300 kg/hm2配施有机肥的活性最高,其余指标均以施氮量N 150 kg/hm2配施有机肥处理效果最佳。3) 施氮量、有机肥、冬小麦生育期显著影响土壤蔗糖酶、碱性磷酸酶、过氧化氢酶和脲酶活性,施氮量和有机肥的交互效应显著影响碱性磷酸酶活性,施氮量和冬小麦生育期的交互效应显著影响土壤蔗糖酶、碱性磷酸酶和过氧化氢酶活性,有机肥和冬小麦生育期的交互效应显著影响土壤碱性磷酸酶和过氧化氢酶活性,施氮量、有机肥和冬小麦生育期三者的交互效应显著影响土壤蔗糖酶活性。4) 相关分析表明,土壤碱性磷酸酶与有机质间、脲酶与速效钾之间均未达显著相关水平,土壤蔗糖酶、碱性磷酸酶、过氧化氢酶和脲酶与有机质、全氮、有效磷、速效钾均呈显著或极显著正相关。【结论】土壤养分、酶活性和冬小麦产量之间密切相关,在施用有机肥30 t/hm2的基础上配施氮肥N 150 kg/hm2,有利于增强黄土高原南部半湿润易旱区冬小麦土壤生态系统的可持续性。     

Einfluß unterschiedlicher Düngungsarten auf das potentielle Stickstoff-Fixierungsvermögen (Acetylen-Reduktionstest) einer Sandparabraunerde

Effect of different fertilizers on the potential N₂-fixing capacity (acetylene-reduction assay) of a sandy orthic luvisol The N₂-fixation capacity of 36 different soil samples, taken from a field trial with 4 fields crops, was tested by the acetylene-reduction-method. Each of the 4 plots was divided into strips. I = mineral fertilizer (NPK), II = stable manure compost, III = stable manure compost with bio-dynamic preparations. These different kinds of fertilizer were given in three amounts of N: 1 = 0,5 × A kg N/ha, 2 = 1 × A kg N/ha, 3 = 1,5 × A kg N/ha. Like the 3 years before in 1984 rye ?Halo”? A = 100, potatoes ?Nicola”? A = 120, red beets ?Rote Kugel”? A = 160, carrots ?Luwal”? A = 120 were cultivated. The soil samples were taken after harvest, dried and sieved. 50 g soil were moistened with a glucose-solution, hatched at 25°C for 24 h and then incubated for another 24 h at the same temperature and an acetylene concentration of 9,23%. The amount of ethylene which had developed after 8 h, 15 h and 24 h was analysed by GC. The acetylene-reduction (AR) of the soils was significantly higher after the cultivation of rye and potatoes compared with carrots and red beets; but always the crops formed the main influence. On an average the organic manured soils showed a higher AR than the mineral fertilized ones. The encouraging effect of the different organic manures was depending on the type of crop.     

Auswirkungen von Bodenverdichtungen auf die Dynamik von Boden- und Düngerstickstoff unter Winterweizen

Effect of soil compaction on the dynamics of soil and fertilizer nitrogen under winter wheat In 1987 and 1988 the effect of severe soil compaction before sowing on the dynamics of soil and fertilizer nitrogen under winter wheat was studied in a field trial at the experimental station of Roggenstein. According to the course of soil nitrate values before winter soil compaction caused a loss of 34 kg N/ha in the first year whereas no such effect could be seen in the second year. During winter vertical nitrate movement was slower on the compacted plots because of the smaller volume of macropores. Without additional N-Fertilizer net N-mineralization during the vegetation period was 22 kg N/ha (32 %) lower in the compacted than in the well structured soil. Total N-yield at harvest was 95 kg N/ha on the control plots and 68 kg N/ha on the compacted plots. The unfavourable soil structure also led to a lower N-fertilizer efficiency, especially in the wet year of 1987, when about 20 % of the fertilizer-N was lost by denitrification whereas in 1988 all fertilizer nitrogen was found in the plant-soil system at harvest. Denitrification on the untreated soil was negligible in both years. The results showed that, besides a weakly developed root system, reduced N-mineralization and increased denitrification losses are responsible for nitrogen deficiency symptoms of plants growing in compacted soils.     

Substance and Energy Balances in the "Static Fertilisation Experiment Bad Lauchstädt"

Data of the "Static Fertilisation Experiment Bad Lauchstädt" were used to identify the effect of different fertiliser application on yield, various energetic parameters as well as on carbon and nitrogen balance of the long-term trial in a selected time period (1991-2000). The fertiliser regimes considered, are neither mineral fertiliser nor farmyard manure (without/without), mineral NPK and no farmyard manure (NPK/without), no mineral fertiliser and 10t ha m 1 a m 1 farmyard manure (without/10), mineral NPK and 10t ha m 1 a m 1 farmyard manure (NPK/10), no mineral fertiliser and 15t ha m 1 a m 1 farmyard manure (without/15), as well as mineral NPK and 15t ha m 1 a m 1 farmyard manure (NPK/15). The farmyard manure was only applicated to root crops. The crop rotation included sugar beets, spring barley, potatoes and winter wheat. In most cases, the treatment NPK/10 yielded in the most favourable results whereas the treatment without/without was the most unfavourable one. Sugar beets were - followed by winter wheat - the most profitable crops, potatoes the most unfavourable one. The fossil energy input was highly variable; it ranged from 4.1 to 24.3GJ ha m 1 a m 1 depending on fertiliser regime and crop. The total yield (based on main products and by-products) varied from 2.1 to 20.1t dry matter ha m 1 a m 1 , corresponding to an energy output between 3.4 and 33.6GJ ha m 1 a m 1 . The energetic parameters energy gain (net energy output) and energy intensity ranged form 25.5 to 315GJ ha m 1 a m 1 and from 143 to 1824MJ GE m 1 , respectively. The carbon balances resulted the highest C gain with the exclusive mineral fertilisation (NPK/without), followed from the treatment NPK/10. The same applies for the nitrogen balances.     

过量施氮对旱地土壤碳、氮及供氮能力的影响

【目的】过量施氮会影响土壤有机碳、氮的组成与数量,进而改变土壤供氮能力,但关于西北旱地长期过量施用氮肥后土壤有机碳、氮及土壤供氮能力变化的研究尚缺乏。本文在长期定位试验的基础上,通过分析不同氮肥水平特别是过量施氮条件下土壤硝态氮,有机碳、氮和微生物量碳、氮的变化,探讨长期过量施氮对土壤有机碳、氮及供氮能力的影响。【方法】长期定位试验位于陕西杨凌西北农林科技大学农作一站。在施磷(P2O5)100kg/hm2的基础上,设5个氮水平,施氮量分别为N 0、80、160、240、320 kg/hm2。重复4次,小区面积40 m2,完全随机区组排列。种植冬小麦品种为小堰22。本文选取其中3处理,以不施氮为对照(N0)、施氮量N 160 kg/hm2为正常施氮(N160),施氮量N 320 kg/hm2为过量施氮(N320),分别于2012年6月小麦收获后和10月下季小麦播前采集土壤样品,进行测定分析。【结果】过量施氮导致下季小麦播前0—300 cm各土层硝态氮含量显著增加,平均由对照的2.8 mg/kg增加到15.5 mg/kg;同时,0—60 cm和0—300 cm土层的硝态氮累积量分别由对照的47.2和108.9 kg/hm2增加到76.5和727.7 kg/hm2。过量施氮也增加了夏闲期间0—300 cm土层土壤有机氮矿化量,由对照的72.4 kg/hm2增加到130.7 kg/hm2。但过量施氮未显著增加土壤的有机碳含量,却显著增加了土壤有机氮含量,过量施氮0—20、20—40 cm土层土壤有机碳分别为9.24和5.39 g/kg,有机氮分别为1.05和0.71 g/kg,较对照增加52.2%和54.3%。同样,过量施氮未显著影响0—20、20—40 cm土层土壤微生物量碳含量,其平均含量分别为253和205 mg/kg,却显著提高了0—20、20—40 cm土层土壤微生物量氮含量,由对照的24.1和7.5 mg/kg提高到43.6和16.1 mg/kg。【结论】过量施氮可以显著增加旱地土壤剖面中的硝态氮累积量、夏闲期氮素矿化量、小麦播前土壤氮素供应量和土壤微生物量氮含量,但对土壤有机碳和微生物量碳没有显著性影响,同时过量施氮增加了土壤硝态氮淋溶风险,故在有机质含量低的黄土高原南部旱地冬小麦种植中不宜施用高量氮肥,以减少土壤氮素残留和农业投入,达到保护环境和培肥土壤的目的。     

Transport of zinc,copper, and lead in a sewage sludge amended calcareous soil

The application of sewage sludge on farmland is practised in many countries since sludge is rich in macro- and micro- nutrients. However, increasing use of sewage sludge on farmland has raised concerns about the potential transport of heavy metals into food chains and groundwater. This study determined for a calcareous soil the effects of sludge application on soil physical properties and transport of zinc (Zn), copper (Cu), and lead (Pb). Secondary anaerobic digested sewage sludge was applied at rates of 0, 25, 50, and 100 t/ha (on a dried weight basis) for four consecutive years and mixed in the top 20-cm of soil. Corn (Zea mays L.) was planted as a spring crop, followed by wheat (Triticum aestivum) as a winter crop. Sludge application increased the dissolved organic matter content and modified the soil structure, increased the soil infiltration rate, saturated hydraulic conductivity, and aggregate stability, and decreased the bulk density. Sludge application greatly increased DTPA (diethylenetriamine pentaacetic acid)-extractable soil metal concentrations to 50 cm depth and significantly to 1 m. In the plots that received four application of 100 t/ha sewage sludge, the mean concentrations of Zn, Cu, and Pb in subsoil increased by 1600, 7, and 4.5 times, respectively, compared with the control. The results indicate that a combination of enhanced soil physical properties, heavy and inefficient irrigation and high organic matter content with heavy metals cause significant metal mobility. High sludge applications pose risks of groundwater and food chain contamination and rates are best restricted to those reflecting the nutrient demand of crops (20 t/ha every 4 to 5 yr or an average of 4 to 5 t/ha/yr).     

有机质、全氮和可矿化氮在反映土壤供氮能力方面的意义

用 2 5个表层土壤样品和 6个土壤 3 6个不同层次的土壤样品研究了可矿化氮与有机质、全氮的关系。可矿化氮由通气培养法测定。研究结果表明 ,不论表层土壤或不同层次剖面土壤中的可矿化氮都与有机质、全氮高度正相关。但是由于可矿化氮与有机质、全氮有自相关存在 ,他们之间的相关有一定的不真实性。而且 ,土壤的可矿化氮并不与全氮或有机质成正比 ,可矿化氮与有机质或全氮的比值因土壤而不同 ,差别很大。特别重要的是 ,可矿化氮对有机质或全氮的比率几乎在一条直线上 ,它们之间的相关性明显高于可矿化氮与有机质或全氮的关系。这些结果显示 ,矿化氮的数量取决于有机质和全氮中的可矿化部分 ,而不是其总量。土壤剖面中累积的硝态氮数量低时 ,作物的吸氮量与可矿化氮的关系远较与有机质或全氮的关系密切 ,更证明了测定可矿化氮有其特定意义 ,有机质、全氮的测定并不能代替可矿化氮的测定。     

Dynamics of the agrochemical fertility parameters of arable soils in the southwestern region of Central Chernozemic zone of Russia

Data of the agrochemical survey of arable soils in Belgorod oblast during the period from 1964 to 2014 have been analyzed. The soil cover mainly consists of typical chernozems (Haplic Chernozems) and leached chernozems (Luvic Chernozems) in the forest-steppe zone and ordinary chernozems (Calcic Chernozems) in the steppe zone. Under long-term agricultural use (from 1964 to 2014), the content of mobile phosphorus in arable soils of the region under study has increased from 55 to 137 mg/kg, and the content of mobile potassium has increased from 105 to 147 mg/kg. During the period of 1976–2014, the share of acid soils has increased from 22.8 to 45.8%, including medium-acid soils from 1.5 to 12.6%. No significant changes in the weighted average content of soil organic matter are revealed for the period from 1985 to 2014. The value of this parameter is within the range of 4.8–5.0%. In the 2010–2014, 95.0% of arable soils belonged to the category of low supplied with mobile sulfur; 99.2, 96.9, 94.1, and 54.4% of soils were poorly supplied with zinc, copper, cobalt, and manganese, respectively. During the same period, the maximum average productivity of the crop area (3710 f. u./ha) was noted at the application of 4.8 t/ha organic fertilizers and 97.9 kg/ha organic fertilizers on the average. The maximum long-term yields of sugar beet (36.8 t/ha) and corn grain (4.97 t/ha) were obtained at the application of relatively low fertilizer rates.     

Nitrogen mineralization in loamy arable soils after increasing the ploughing depth and ploughing grasslands

Abstract. Increasing the ploughing depth and ploughing in grassland has been common in Germany during the past 20 years. Incubation studies were conducted with topsoils from luvisols and gleysols at different times after change of management in order to assess its influence on nitrogen mineralization and its kinetic parameters.
The results show that deep ploughing slows the mineralization of nitrogen. The difference between earlier (1967–72) and more recently (1980–82) deepened topsoil has become smaller after a further three years of cultivation, however. The preceding crops (wheat or sugar beet), the amount of N fertilizer as well as clay and nitrogen contents cause a variation in N mineralization. The results indicate a continuing approach of an'equilibrium'organic matter and nitrogen content. The enrichment capacity of intensively managed soils may be replenished within 10 years.
Gleysols formerly under grass mineralize more nitrogen than'traditionally'ploughed soils, even 27 years after the ploughing-in. While nitrogen from easily decomposable materials decreases within the first 10 years, the resistant fraction is a long-lasting determinant for N mineralization. Both processes need to be considered when applying fertilizer to minimize nitrate leaching.     

ACCUMULATION OF ORGANIC MATTER IN A CHRONOSEQUENCE OF SOILS DEVELOPED ON WIND-BLOWN SAND IN NEW ZEALAND

A study was made of the amounts and distribution of C, N, S, and organic P accumulated over a period of 10 000 years of soil development on wind-blown sand. After initial rapid rates of accumulation of C, N, and organic P during the first 1000 years, subsequent rates of gain were slower, but steady states for C, N, and S had still not been reached after 10 000 years. Sulphur declined during the first 50 years of soil development but then increased in a parallel fashion to organic C. During 10 000 years, gains of organic C, total N, total S, and organic P were 204 000, 9800, 1180, and 1170 kg/ha m profile, respectively. Gains in total N and S in the older soils are readily accounted for by returns in precipitation. Pronounced changes in soil organic matter composition during 10 000 years are reflected in the widening of the C/N ratio (8 to 20) and the C/organic P ratio (39 to 159).     

Über die Sorptionseigenschaften von Waldböden bezüglich gelöster organischer Substanzen

About the sorption of dissolved organic matter to forest soils This investigation characterizes the major forest soils of the temperate climatic zones (leptosols, vertisols, cambisols, luvisols, podzols, stagnosols, gleysols) as sorbents for dissolved organic matter (DOM). Sorption isotherms were obtained for 135 soil horizons from 36 profiles. When solutions containing no DOC were added, the release of dissolved organic carbon (DOC) was highest for horizons rich in organic C (A and Bh horizons). In subsoil horizons DOC release was much lower. Most of the investigated top soils (A and E horizons) and Bh, Bg, and C horizons showed a weak DOC sorption. This was caused by low contents of sorbents (clay and sesquioxides) and/or high contents of organic C. Organic C seems to reduce the DOC sorption by occupying binding sites. Subsoils rich in clay and sesquioxides like Bs, Bt, and Bw horizons showed a strong retention of DOC. Under the aerobic conditions of the experiments, some of the subsoils of stagnosols and gleysols also showed a strong sorption of DOC. However, in sorption experiments conducted after an anaerobic incubation, the DOC sorption decreased significantly.