Incubation experiments on nitrogen mineralization in loess and sandy soils

Summary In aerobic incubation experiments, nitrogen mineralization was investigated in agricultural loess and sandy soils. Fresh, fieldmoist samples were used for incubation. Using an optimization procedure the N-mineralization was split into two nitrogen fractions: A resistant, slowly decomposable organic N-fraction (index rpm) and a fast decomposable N-fraction (index dpm).Loess- and sandy soils showed similar mean reaction coefficients for N-mineralization. The results also indicated that the amount of mineralizable nitrogen in the resistant N-fraction depended directly on clay content.Soil sampling at different times during crop growing period gave different mineralization amounts and courses.Effect of added plant residues on N-mineralization, was also studied by incubation. Variation of type and quantity of added residues changed the net N-mineralization in a characteristic way: Sugar beet leaves, added in minced form, caused an increase in mineralization; while straw caused a temporary immobilization, followed by remineralization.Incubation experiments on undisturbed soil columns showed nearly linear mineralization with time.This paper was presented in part at the 1983 Congress of the German Soil Science Society held at Trier.     

人工油松林（Pinus tabulaeformis）恢复过程中土壤微生物生物量C、N的变化特征

采用时空替代法,选取15a（PF15）、25a（PF25）、30a（PF30）的人工油松林作为样地,并选取灌丛作为参考植被,研究了植被恢复过程中土壤微生物生物量C、N以及土壤养分的变化特征,同时探讨了它们之间的相互关系。研究结果表明随着恢复的进行,土壤质量得到了改善,主要表现为有机碳、全氮、粘粒含量、土壤含水量的上升和pH值、容重的下降。土壤微生物生物量C、N分别在155.00~885.64mg/kg和33.73~237.40mg/kg的范围内变化。土壤微生物生物量C、N在植被恢复的初期显著低于灌丛,而后随着恢复的进行逐步增长。土壤微生物生物量C、N与植被恢复时间的相关性没有达到统计学上的显著水平,但是土壤微生物生物量C与土壤有机碳、全氮、全磷呈显著正相关,这表明植被恢复过程中土壤微生物生物量与土壤养分状况关系密切,植被恢复通过改善土壤养分状况间接地影响土壤微生物生物量的变化。Cmic/TOC在1.38%~4.75%的范围内变化。Cmic/TOC随着植被恢复不断下降,Cmic/TOC与植被恢复时间和土壤有机碳呈显著负相关,这表明植被恢复过程中,惰性有机质积累导致供应土壤微生物的活性有机质减少,Cmic/TOC同时受土壤有机质的数量和质量影响。     

26年长期施肥对土壤微生物量碳、氮及土壤呼吸的影响

研究长期小麦连作施肥条件下土壤微生物量碳、氮,土壤呼吸的变化及其与土壤养分的相关性。以陕西长武长期定位试验为平台,应用氯仿熏蒸-K2SO4提取法、碱液吸收法和化学分析法分析了长达26a不同施肥处理农田土壤微生物量碳、微生物量氮和土壤呼吸之间的差异及其调控土壤肥力的作用。长期施肥及种植作物,均能提高土壤微生物量碳、氮含量,尤其是施用有机肥,土壤微生物量碳、氮含量高于单施无机肥的处理,土壤呼吸量也提高15.91%—75.73%,而施用无机肥对于土壤呼吸无促进作用。土壤微生物生物量碳氮、土壤呼吸与土壤有机质、全氮呈极显著相关。长期有机无机肥配施可以提高土壤微生物量碳氮、土壤呼吸,氮磷肥与厩肥配施对提高土壤肥力效果最好。微生物量碳氮及土壤呼吸可以反映土壤质量的变化,作为评价土壤肥力的生物学指标。     

N-mineralization in Löss-Parabrownearthes: Incubation experiments

Summary Nitrogen mineralization in Löss-Parabrownearthes was studied in long-term incubation experiments at different temperatures. Results obtained were used to optimize the parameters of a first-order kinetic model for N-mineralization of these soils: average reaction coefficients obtained by incubationat 35°C are 0.00737±0.00081 per day for the old organic material, and 0.25±0.07 per day for the fresh organic material.The mineralizable nitrogen of the fresh organic material at the beginning of march amounts to about 90±20 kg N/(ha*30 cm), independent of the kind of preceding crop. Temperature dependence of mineralization was estimated roughly. Attempts to simplify the procedure of evaluation of these parameters are described.Aqualfs and Udalfs according to the 7th approximation.     

湿地土壤微生物功能多样性及碳氮组分对长期氮输入的响应

氮输入对湿地生态系统碳氮循环具有重要影响,研究湿地土壤微生物功能多样性及碳氮组分对氮输入的响应,对于明确湿地土壤碳氮循环微生物驱动机制具有重要意义。依托长期野外氮输入模拟试验,利用Biolog-ECO微平板技术,分析不同浓度氮输入:N1(6 g N m^-2 a^-1)、N2(12 g N m^-2 a^-1)和N3(24 g N m^-2 a^-1)对湿地土壤表层(0-15 cm)和亚表层(15-30 cm)微生物碳源代谢活性、功能多样性和碳氮组分的影响。结果表明:N2处理显著提高了亚表层土壤微生物碳源代谢活性和McIntosh指数,N3处理显著降低了表层土壤微生物Shannon指数和Shannon-evenness指数。随氮输入浓度增加湿地表层土壤微生物对糖类的利用率显著降低,N3处理表层土壤微生物对胺类的利用率以及亚表层土壤微生物对醇类的利用率显著提高。N1处理显著提高了湿地表层土壤全氮和微生物量碳含量;N2、N3处理显著提高了土壤铵态氮、硝态氮含量;N3处理显著降低了土壤pH值。湿地土壤pH、总碳、溶解性有机碳含量是影响微生物碳源代谢活性和功能多样性的重要因素,土壤溶解性有机碳、铵态氮、全氮含量、含水率是影响微生物碳源利用变化的主要因子。     

The impact of long-term nitrogen addition on microbial community composition in three Hawaiian forest soils

We evaluated the microbial communities in three Hawaiian forest soils along a natural fertility gradient and compared their distinct responses to long-term nitrogen (N) additions. The sites studied have the same elevation, climate, and dominant vegetation, but vary in age of development, and thus in soil nutrient availability and nutrient limitation to plant growth. Fertilized plots at each site have received 100 kg ha year(-1) N addition for at least 8 years. Soil parameters, water content, pH, and ammonium and nitrate availability differed by site, but not between control and N-addition treatments within a site at the time of sampling. Microbial biomass also varied by site, but was not affected by N addition. In contrast, microbial community composition (measured by phospholipid analysis) varied among sites and between control and N-addition plots within a site. These data suggest that microbial community composition responds to N addition even when plant net primary productivity is limited by nutrients other than N. This may have implications for the behavior of forests impacted by atmospheric N deposition that are considered to be "nitrogen saturated," yet still retain N in the soil.     

Soil nitrogen dynamics in a holm oak forest

Soil nitrogen (N) dynamics were studied in a dense, holm oak (Quercus ilex ssp. ilex) stand in the Montseny mountains to determine annual and seasonal patterns of N availability and uptake in an undisturbed Mediterranean forest on acidic soil. Soil mineral N content, net N mineralization (NNM), and net nitrification (NN) were determined by monthly sampling at two soil depths followed by in situ incubation in polyethylene bags. NNM per unit of soil mass was much higher at 0–5 cm than at 5–20 cm (annual means 24 and 2.5 mg N/kg, respectively) but on an area basis NNM was similar at both depths. A total of 80 kg N/ha/yr were mineralized from the first 20 cm of soil. NN amounted to only 9% of the annual NNM (7.5 kg N/ha/yr) and it occurred only in the upper 5 cm. NNM was maximum in June and July, while the NN peaked in May. Despite favourable soil temperature and moisture, NNM was negative in autumn because of microbial immobilization. Seasonal and depth variations of NNM appeared to be controlled more by substrate quality than by organic matter quantity, temperature or moisture. NN was not limited by ammonium availability. Calculated N uptake amounted to 91 kg/ha yr, peaking in June and July. The investigated stand showed a moderately high N availability, but ammonium was the major form of mineral N supply for holm oak.     

Greater soil microbial biomass loss at low frequency of N addition in an Inner Mongolia grassland

低频率的氮添加使内蒙古草原土壤微生物生物量碳出现更大幅度下降 土壤微生物生物量在生物地球化学循环过程中至关重要,是土壤碳固持的前体物质。人为氮输入深刻地改变了草地土壤微生物生物量。然而,传统氮沉降模拟实验仅通过低频率的氮添加进行,与持续高频率的自然氮沉降相比,对土壤微生物生物量的影响可能存在差异。不同频率的氮添加对土壤微生物生物量的影响尚缺乏可靠的数据支撑。本研究通过在不同的氮添加速率(0–50 g N m−2 yr−1)下,控制氮添加频率(每年2次和12次),研究了土壤微生物生物量碳对不同氮添加频率的响应。研究结果表明,在两种氮添加频率下,随着施氮水平的提高,土壤微生物生物量碳逐渐降低。然而,在低施氮频率下,土壤微生物生物量的下降幅度更大,这说明传统的氮添加实验可能高估了氮沉降对土壤微生物生物量的影响。在低施氮频率下,土壤酸化、无机氮积累、碳氮失衡、地下净初级生产力分配减少和真菌细菌比例降低等情况加剧,导致微生物生物量出现较大幅度下降。在未来研究中,为可靠预测氮沉降对草地生态系统土壤微生物功能和碳循环的影响,不仅要考虑氮添加的剂量,还需要考虑氮添加的频率。     

Leaching losses of nitrogen and potassium in polders reclaimed from Lake Ijssel

Summary Mineral nitrogen and potassium lost from the Eastern Flevoland polder and from the North Eastern polder were estimated at regular intervals by determining the amounts of soluble nitrogen and potassium in the water which had been admitted by locks and inlets and discharged by pumping stations and subtracting nitrogen and potassium added in the rain. From 1959 to 1966 the nett annual losses of nitrogen in the discharged water from various pumping stations in Eastern Flevoland ranged from 18.9 to 33.2 (average 25.2) kg N per ha. Similarly in the North Eastern polder from 1963 to 1966 the nett annual losses ranged from 16.7 to 33.2 (average 22.1) kg N per ha. Rainfall added annually between 4.8 and 11.8 (average 8.6) kg N per ha to both polders. Nett losses from Eastern Flevoland ranged from 9.2 to 21.9 (average 15.8) kg per ha and from the North Eastern polder from 10.1 to 24.0 (average 14.9) kg N per ha, annually. Drainage water contained principally nitrate nitrogen, whereas the discharged water in many cases contained both ammonium and nitrate nitrogen, and often more ammonium than nitrate, presumably because the composition of the mineral nitrogen in the waterways is changed by the growth and death of algae. From 1962 to 1966 the discharged water removed potassium from the Eastern Flevoland polder in amounts ranging from 105 to 226 (average 162) kg K per ha annually. During 1963–1964, amounts lost from the North Eastern polder ranged from 47 to 71 (average 59) kg K per ha each year. The rain added from 4.5 to 10.7 (average 6.9) kg K per ha annually to both polders. Nett losses from Eastern Flevoland ranged from 99 tot 219 (average 156) kg K per ha and from the North Eastern polder from 41 to 67 (average 54) kg K per ha annually.     

种植密度与施氮量对麦茬复种饲料油菜土壤微生物活性的影响

通过田间小区试验,研究了不同油菜种植密度与施氮肥对麦茬复种饲料油菜耕层土壤(0～5 cm)微生物活性的影响.结果表明,复种油菜能显著或极显著性提高耕层土壤微生物量碳(C_mic)、土壤微生物量氮(N_mic)、土壤细菌数(SBN)、土壤真菌数(SFN)和土壤放线菌数(SAN),而显著降低土壤微生物量碳/氮比(C_mic/N_mic).随油菜种植密度的提高,耕层C_mic、C_mic/N_mic、SBN呈逐渐增加态势,而N_mic、SAN呈降低趋势.随着施氮肥梯度增加,耕层SFN显著提高,C_mic和N_mic呈先降低后增加再降低趋势,以1 000 kg·hm^-2施肥处理最高.SFN和收获期SAN为先降低后升高,苗期SAN则为先升高后降低.相同处理油菜收获期各土壤微生物活性指标均高于苗期,而600 kg·hm^-2苗期SAN则相反.SBN和SAN与C_mic、N_mic呈正相关,与C_mic/N_mic呈负相关,SFN与C_mic、N_mic及C_mic/N_mic之间均无明显相关性.