In situ acetylene-ethylene assay of biological nitrogen fixation in lowland rice soils

Summary An in situ device for assaying biological nitrogen fixation in flooded rice soils, using the acetylene reduction method, was developed. Diurnal variations in acetylene reduction by an inoculated field plot and by laboratory-grown cultures of nitrogen-fixing algae showed a prominent single-peak pattern of nitrogenase activity. The peak occurred at mid-day for laboratory-grown algae and at late afternoon for the algae grown in the field plot. Some nitrogenase activity was noted during the night. Acetylene reduction studies in rice fields of Albay province, Philippines, showed an estimated fixation of 18.5 to 33.3 kg N/ha each cropping season for the fields of Puro soil and 2.3 to 5.7 kg N/ha each cropping season for the fields of Santo Domingo soil. re]19751202     

Loss and recovery of nitrogenase in Abuts incana nodules exposed to low oxygen and low temperature

The possibility that respiration limits oxygen access to nitrogenase was tested by artificially upsetting the balance between oxygen consumption (respiration) and oxygen influx (diffusion). Argon treatment of the nodulated root system on intact plants stopped in vivo nitrogenase activity almost completely. Upon return to air, nitrogenase activity was very low and recovered gradually to full activity after about 5 h. In vitro measurements on nodule homogenates indicated that active nitrogenase was lost upon the shift from low (argon) to normal (air) oxygen. Maintenance of nodulated root systems at low temperature (2°C) inhibited both respiration and in vivo nitrogenase activity. Upon return to normal temperature (22°C), oxygen uptake recovered very rapidly, but nitrogenase activity recovered only gradually to full activity after about 5 to 6 h. Again, loss of active nitrogenase could, at least partly, explain the reduced in vivo nitrogenase activity. The effects from a temporarily impaired balance between oxygen consumption and oxygen influx thus point to the importance of respiration for limiting oxygen access to nitrogenase.     

Analysis of factors affectingin situ nitrogenase (C2H2) activity ofGalega orientalis,Trifolium pratense andMedicago sativa in temperate conditions

Summary A practical fibreglass cylinder-plastic bag system has been designed for making acetylene reduction assays in the field. Thein situ assay was used to determine seasonal patterns of nitrogenase activity for the perennial forage legumesGalega orientalis, Trifolium pratense andMedicago sativa grown under stadard management in southern Filand (60° north). Nitrogenase activity was still detected in the field plots in November, when soil temperature was 1.5°C and air temperature 0.5°C. The acetylene reduction data from weekly measurements were analyzed for correlation with plant growth rate and short-term fluctuations of environmental factors. Generally, there was a good correlation between nitrogenase activity and plant growth rate. Residual fluctuations in activity were only correlated with environmental factors in one case. The nitrogenase activity ofM. sativa was dependent on air temperature in addition to growth rate. Thus, the nitrogen fixing systems in these forage legumes seem to be an integrated part of the plants, being fairly insensitive to short-term environmental changes.Dedicated to Prof. Helge Gyllenberg on the occasion of his 60th birthday.     

Effect of Temperature on the Nitrogenase Activity of Intact and Detached Nodules in Lotus and Stylosanthes

Temperature and plant age influenced the nitrogenase activityof Lotus and Stylosanthes nodules. Time course studies usingnodulated plants in closed vials showed a decline in activityafter 48 h; regassing with 10% (v/v) acetylene in air partiallyrestored the activity. Transfer of plants from 15, 20, 25, and30 ?C to 40 ?C immediately stopped activity; this was completelyrestored within 1 h after return to original temperatures. Detached nodules cultured on nitrogen-free agar medium exhibiteda sucrose concentration (2–8%, w/v)-dependent nitrogenaseactivity at each temperature. With 6% sucrose prolonged activity,up to 96 h, was obtained. Decline in nitrogenase activity indetached nodules was due partly to exposure to air during excisionand transfer to the medium.     

沈阳城市森林小气候特征的研究

研究了沈阳城市森林不同生长期小气候温湿日变化特征.结果表明,城市森林不同生长期气温日变化趋势是早晨气温最低、午后气温最高,但受森林生态环境的影响,最高峰比太阳辐射峰值迟滞约2 h.一年四季气温日变幅为森林停止生长期(休眠期)＞生长季前期＞生长季后期＞生长季中期.森林生长季前期、中期、后期土壤温度为白天高于夜间,而停止生长期(休眠期)为夜间高于白天.不同生长期土温日振幅为上层(20 cm)＞中层(40 cm)＞下层(80 cm),而同一层不同生长期的土温日振幅为土层深20 cm时,生长季前期＞生长季后期＞停止生长期(休眠期)＞生长季中期;土层深＞40 cm(80 cm)时,生长季前期＞停止生长期(休眠期)＞生长季后期＞生长季中期.城市森林空气相对湿度日变化与气温和地温日变化则夜间的空气相对湿度高于白天,但不同生长期相对湿度值日变化为生长季中期＞生长季后期＞停止生长期(休眠期)＞生长季前期.     

Upper temperature limits for growth and diazotrophy in the thermophilic cyanobacterium HTF Chlorogloeopsis

The effect of temperature and oxygen on diazotrophic growth of the thermophilic cyanobacterium HTF (High Temperature Form) Chlorogloeopsis was investigated using cells grown in light-limited continuous culture at a dilution rate of 0.02 h^-1. Diazotrophy was more sensitive to elevated temperatures than growth with combined nitrogen. The maximum temperature for growth of cultures gassed with CO₂-enriched air was more than 55 °C but less than 60 °C with N₂ as the sole nitrogen source, but between 60°C and 65°C when nitrate was present in the medium. The effect of temperature on nitrogenase activity, photosynthesis and respiration in the dark was determined using cells grown at 55°C. Maximal rates of all three processes were observed at 55°C and rates at 60°C during shortterm incubations were not less than 75% of the maximum. However, nitrogenase activity at 60°C was unstable and decayed at a rate of 2.2 h^-1 under air and at 0.3 h^-1 under argon. Photosynthesis and respiration were more stable at 60°C than anoxic nitrogen fixation. The upper temperature limits for diazotrophic growth thus seem to be set by the stability of nitrogenase.Abbreviations chl chlorophyll a - DCMU N-(3,4-dichlorophenyl) N,N-dimethylurea - Taps N-tris(hydroxymethyl)methyl-3-aminopropanesulfonic acid     

Reproductive Development and Nitrogen Fixation in Soybean (Glycine max [L.] Merril)

Gomes, M. A. F. and Sodek, L. 1987. Reproductive developmentand nitrogen fixation in soybean (Glycine max (L.) Merril).—J.exp. Bot. 38: 1982–1987. Nitrogenase activity (acetylene reduction) was measured duringthe growth cycle of soybean plants induced to flower at twodifferent ages. The decline in nitrogenase activity towardsthe end of the cycle was clearly associated with pod-fillingfor both flowering dates when plants were cultivated under lowerlight and temperature conditions (out of season). Under higherlight and temperature conditions (normal growing season) thedecline was independent of the flowering date. Furthermore,the timing of the decline was not altered when plants were maintainedunder long-day (vegetative) conditions nor when flowers wereremoved. It is suggested that under more favourable growth conditionsthe diversion of assimilates by the fruits is not the primarycause of the decline in nodule activity, but competition bythe fruits may be important when the production of photo-assimilatesis more limited. Key words: Glycine max, nitrogenase, source-sink     

Activity and expression of nitrogenase in Rhodobacter capsulatus under aerobiosis in the dark and in the light

Rhodobacter capsulatus was grown chemotrophically in the dark in oxygen-regulated chemostat culture and in the presence of limiting amounts of fixed N. When the oxygen partial pressure was varied, in situ nitrogen fixation occurred only at 1% of air saturation of the medium. By contrast, nitrogenase proteins and their activity measured in the absence of oxygen could be detected up to 30% of air saturation. This revealed that expression of nitrogenase is much less sensitive toward oxygen than the in situ function of the enzyme. At oxygen partial pressures > 1% of air saturation, the degree of modification of the Fe protein of nitrogenase was increased. Light was of no stimulatory effect on both the activity and the expression of nitrogenase. This holds true for growth at 1% or 5% of air saturation. At 5% of air saturation, however, high illumination enhanced the inhibitory effect of oxygen on nitrogenase formation.     

Day-to-day variation in nitrogenase activity of Alnus incana explained by weather variables: a multivariate time series analysis

A modelling system is described that indicates the extent to which day-to-day variations in nitrogenase activity in young Alnus incana (L.) Moench, grown in defined conditions in the field, may be affected by weather conditions both during and prior to the day of measurement. Nitrogenase activity (acetylene reduction activity, ARA) was measured weekly on intact field-grown grey alder (A. incana) plants, 0.15–0.42 m tall at planting, nodulated with Frankia. The measurements were done at noon on two groups of plants in 1987 and on two other groups in 1988. Each group was made up of five or six plants. Seven weather variables: daily sunshine hours, daily mean, maximum and minimum air temperature, daily mean and 1300 h relative humidity, and daily rainfall were used. The relation between log(ARA/leaf area) and the weather variables were analysed using a PLS model (partial least squares projection to latent structures). The advantage of PLS is that it can handle x-variables that are correlated. Data from 1987 were chosen as a training set. Multivariate PLS time series analysis was made by adding, in a stepwise manner, the weather data up to 5 d before the day of measurement. This procedure gave six models with n * 7 x-variables (n= 1–6). With the models from the time series analysis of 1987 data, true predictions of ARA per leaf area were made from weather data 1988 (test set 1) and from ‘early-season’ weather data from 1987 and 1988 (test set 2). The variation in ARA/leaf area could be predicted from the weather conditions. The predictions of the two test sets improved when the weather conditions one and two days before the day of measurements were added to the model. The further addition of weather data from 3 to 5 d before the day of measurement did not improve the model. The good predictions of ARA/leaf area show that the alders responded to the variable weather conditions in the same way in 1988 as in 1987, despite the ten-fold difference in size (leaf area) at the end of the growing season. Among the weather variables, air temperature and the daily sunshine hours were positively correlated to ARA, while relative air humidity and rainfall were negatively correlated to ARA. The daily minimum temperature and rainfall appeared to have least impact on ARA. By use of PLS, we could extract information out of a data set containing highly correlated x-variables, information that is non-accessible with conventional statistical tools such as multiple regression. When making measurements of nitrogenase activities under field conditions, we propose that attention should be paid to the weather conditions on the days preceding the day of measurement. The day-to-day variation in nitrogenase activity is discussed with reference to known effects of stress factors under controlled conditions.     

台湾相思结瘤固氮与吸氢酶活性研究

台湾相思的根系具有多年生的根瘤,根瘤初发生时球状,以后发育成分叉瘤和扇状瘤。根瘤固氮活性因苗龄、成熟度不同而有明显差异。环境条件影响结瘤及固氮活性。15℃时结瘤受到明显抑制,固氮作用最适温度条件是25～30℃。光照不足降低根瘤固氮活性。短期轻度干旱不影响根瘤固氮活性,但持续干旱使固氮活性明显下降。pH4.5～8.5条件能正常结瘤,pH5.5时结瘤最好。根瘤固氮作用时不释放H_2,具有较高的吸氢酶活性,在固氮反应系统中加入5％的H_2,能提高根瘤固氮活性。     

Impact of altitudinal gradients on energetics and efficiencies of N<Subscript>2</Subscript>-fixation in alder–cardamom agroforestry systems of the eastern Himalayas

The impact of altitudinal gradients on the performance of alder–cardamom agroforestry systems was analyzed on nitrogenase activity, N₂-fixation efficiency, and stand energetics and efficiencies in the eastern Himalayas. Acetylene reduction (AR activity) measurements showed that nitrogenase activity considerably increased with advancing altitudes from 500 to 800 m to a peak at 900–1,200 m. AR activity was fairly high, between 1,300 and 1,700 m, and sharply decreased in the stands between 1,800 and 2,100 m. AR activity increased in the growing season and peaked in the rainy season. This significantly coincided with cardamom flowering during the onset of growing season to full fruiting stage at peak activity period. AR activity was dependent on soil temperature and moisture and showed a positive relationship. Nodule moisture was also a limiting factor for AR activity and showed a positive correlation. Diurnal changes showed a marked variation with highest AR activity between 8 and 12 h. The performance of commercial cardamom crop is dependent on the associated shade trees. Yield potential significantly coincided with the rate of N₂-fixation both at age chronosequence and altitudinal gradients. The management comprises growing large number of alder until 10 years and thinning, and gap filling of cardamom up to 20 years. Such maintenance caused non-equilibrium conditions that favored systems efficiency and excellent production until 20 years. System efficiency sharply declined at low rates of N₂-fixation, AR activity, root nodule production, and agronomic yield due to the influence of stand age and altitudinal gradients. Agroforestry stands at 900–1,700 m were more energy cost-effective due to the lower energy required for per-kg N-fixation with high N supply (115–155 kg ha⁻¹) confirming functionally efficient than those stands at extreme higher and lower altitudinal ranges. Therefore, replantation of alder and cardamom and phase wise agroforestry rotation after 20 years could be an ecologically and economically sustainable management practice.     

Nitrogen-Fixing Activity in Peat Soils from a Raised Bog

The nitrogenase (acetylene reductase) activity in monolithic and minced peat samples was found to be low, no more than 0.014–0.022 mg N/(kg h). Incorporation of the ¹⁵N₂ isotope into organic compounds of peat soil was 2.71–8.13 mg N/kg over 15 days. The nitrogen-fixing activity was the highest in a 10- to 20-cm layer of soil and much lower in the upper (under green moss) and deeper (20- to 30-cm) layers. The addition of glucose to soil samples stimulated nitrogen fixation considerably after 18–26 h. The maximum nitrogenase activity (3.5–3.8 mg N/(kg h)), observed after 60–70 h, coincided with the peak of respiratory activity. A repeated addition of glucose after its exhaustion increased nitrogenase activity, without a lag period, to 8.5 mg N/(kg h). Investigation of the effect of environmental factors (temperature, pH, aeration, and light intensity) on potential nitrogen-fixing activity in peat samples revealed that nitrogen fixation could proceed in a wide range of pH values (from 3.0 to 7.5) and temperatures (from 5 to 35°C). The nitrogen-fixing bacteria belonging to different trophic groups were enumerated by using nitrogen-free media with pH values and mineralization levels close to those in situ. In samples of peat soil, diazotrophic methanol-utilizing bacteria prevailed (2.0–2.5 × 10⁶ cells/g); the second largest group was facultatively anaerobic bacteria of the family Enterobacteriaceae.     

Nitrogen fixation by the unicellular cyanobacterium Gloeothece. Nitrogenase synthesis is only transiently repressed by oxygen

Abstract The extent of recovery of nitrogenase activity of Gloeothece transferred from an atmosphere of O₂ to air depended on the duration of exposure to O₂. Activity recovered at increasing rates after up to 24 h exposure to O₂ and a lag before detection of activity, present after short (1 h) exposure times, disappeared with longer exposures. Synthesis of nitrogenase de novo was implicated, since chloramphenicol, tetracycline, or repressive levels of NH⁺₄, prevented recovery of activity. Specific radioimmunoassay of the rate of synthesis of the MoFe protein of nitrogenase under O₂ correlated well with the activity measurements, and indicate that a shift from air to O₂ only transiently represses nitrogenase synthesis.     

Further Errors in the Acetylene Reduction Assay: Effects of Plant Disturbance

A flow-through gas system was used to study the effects of disturbanceon nitrogenase (acetylene reduction) activity of nodulated rootsystems of soyabean (Glycine max) and white clover (Trifoliumrepens). Detopping plus removal of the rooting medium (by shaking)produced a substantial decrease in maximum nitrogenase activity.This response is due to a reduction in oxygen flux to the bacteroidscaused by an increase in the oxygen diffusion resistance ofthe nodule. The decrease in maximum nitrogenase activity wasmuch smaller for roots subjected to detopping only. Thus, theeffect of root shaking is more important than that of shootremoval. The effect of detopping plus root shaking on nitrogenase activityoccurred whether the plants were equilibrated and assayed at25°C or 15°C. However, the effect of disturbance onthe oxygen diffusion resistance of the nodules, and thus onnitrogenase activity, was greater at the higher temperature.At the lower temperature the oxygen diffusion resistance ofthe nodules had already been increased in response to the reducedrequirement for oxygen. These nodules were less susceptibleto the effects of disturbance. Thus, comparisons of the effectsof equilibration temperature on nitrogenase activity produceddifferent results depending on whether intact or disturbed systemswere used. With intact systems activity was lower at the lowertemperature but with detopped/shaken roots the lowest activityoccurred at the higher temperature. It is concluded that the use of detopped/shaken roots can producesubstantial errors in the acetylene reduction assay, which makesthe assay invalid even when used for comparative purposes. However,comparisons with rates of ¹⁵N₂ fixation and H₂ production showthat accurate measurements of nitrogenase activity can be obtainedfrom maximum rates of acetylene reduction by intact plants ina flow-through gas system. The continued use of assay proceduresin which cumulated ethylene production from disturbed systemsis measured in closed vessels must be questioned. Key words: Nodules, acetylene, nitrogenase activity     

Nitrogen-fixing activity in peat soils from a raised bog

The nitrogenase (acetylene reductase) activity in monolithic and minced peat samples was found to be low, no more than 0.014-0.022 mg N/(kg h). Incorporation of the 15N2 isotope into organic compounds of peat soil was from 2.71-8.13 mg N/kg over 15 days. The nitrogen-fixing activity was the highest in a 10-20 cm layer of soil and much lower in the upper (under green moss) and deeper (20-30 cm) layers. The addition of glucose to soil samples stimulated nitrogen fixation considerably after 18-26 h. The maximum nitrogenase activity (3.5-3.8 mg N/(kg h)) observed after 60-70 h coincided with the peak of respiratory activity. A repeated addition of glucose after its exhaustion increased nitrogenase activity without a lag period to 8.5 mg N/(kg h). Investigation of the effect of environmental factors (temperature, pH, aeration, and light intensity) on potential nitrogen-fixing activity in peat samples revealed that nitrogen fixation could proceed in a wide range of pH values (from 3.0 to 7.5) and temperatures (from 5 to 35 degrees C). The nitrogen-fixing bacteria belonging to different trophic groups were enumerated by using nitrogen-free media with pH values and mineralization levels close to those in situ. In samples of peat soil, diazotrophic methanol-utilizing bacteria prevailed (2.0-2.5 x 10(6) cells/g); the second largest group was facultatively anaerobic bacteria of the family Enterobacteriaceae.     

Comparison of Nitrogen Fixation for North- and South-facing <Emphasis Type="Italic">Robinia pseudoacacia</Emphasis> Stands in Central Korea

The nitrogenase activity, root nodule biomass, and rates of nitrogen (N) fixation were measured in 25-year-old pure north- and south-facing Robinia pseudoacacia stands in an urban forest of Seoul (Kkachisan Mountain) in central Korea. The nitrogenase activity was estimated using an acetylene reduction (AR) assay, which showed an increasing trend during the early growing season, with sustained high rates from June through to September with a decrease thereafter. July had the highest nitrogenase activity rate (micromoles C₂H₄ per gram dry nodule per hour), averaging 95.8 and 115.1 for the north- and south-facing stands, respectively. The maximum root nodule biomass (kilograms per hectare) was 45.7 and 9.1 for the north- and south-facing stands in July, respectively. The AR rate appeared to be strongly correlated to the soil temperature (r ² = 0.68, P < 0.001) and soil pH (r ² = 0.59, P < 0.001) while root nodule biomass was correlated to the soil temperature (r ² = 0.36, P < 0.01) and water content (r ² = 0.35, P < 0.05). The soil temperature showed clear differences between seasons, while there was a significant difference in soil pH, organic matter, total N concentrations, and available phosphorus between the north- and south-facing stands. The N₂ fixation rates during the growing season varied from 0.1 to 37.5 kg N ha⁻¹ month⁻¹ depending on the sampling location and time. The annual N₂ fixation rate (kg N per hectare per year) was 112.3 and 23.2 for the north- and south-facing stands, respectively. The differences in N₂ fixation rate between the two stands were due mainly to the differences in total nodule biomass.     

湿地生态系统土壤温度对气温的响应特征及对CO2排放的影响

通过2年的野外定位观测,研究了沼泽湿地土壤温度对气温变化的响应特征,以及土壤温度对沼泽湿地植物 土壤系统CO₂排放的影响,并对CO₂排放的季节性变化进行模拟计算.结果表明,随融冻作用开始,沼泽湿地土壤温度对气温变化的响应强度不断增大,根层土壤温度与气温间呈显著指数关系（R²=0.94,P<0.01）,但不同深度土壤温度对气温变化的响应强度存在一定的差异,表现为随土壤深度的增加,二者之间的相关系数变小,土壤温度对气温的响应强度减弱.沼泽湿地植物 土壤系统CO₂排放与根层土壤温度有关,二者呈显著指数相关关系（R²=0.84,P<0.01）,利用模型模拟计算出沼泽湿地2003年生长季植物 土壤系统CO₂排放通量平均值为664.5±213.9 mg·m^-2·h^-1,野外定位观测值为634.0±227.7 mg·m^-2·h^-1,二者之间差值不大,表明利用此方法可以对沼泽湿地生长季CO₂排放进行估算.     

南亚热带森林演替过程中小气候的改变及对气候变化的响应

区域水热格局变化和系统演替深刻影响森林内部小气候,不同演替阶段森林内部水热环境对气候变化的响应和反馈作用有待进一步认识和评估。以南亚热带地区的3种不同演替阶段代表性森林生态系统统(人工恢复的马尾松针叶林(Pinus massoniana coniferous forest,PF)、马尾松针阔叶混交林(mixed Pinus massoniana/broad-leaved forest,MF)和季风常绿阔叶林(monsoon evergreen broad-leaved forest,MEBF))为研究对象,通过分析其林内小气候林型间差异以及时间序列上的动态变化,探讨森林系统内部水热环境的改变机理。结果表明:演替驱动下,随着PF→MF→MEBF的正向发展,林内温度条件如气温、土壤温度逐渐降低,林内相对湿度、土壤层及凋落物含水量等水分状况逐步升高。不同林型在"雨热同期"的南亚热带地区其"降温效应"有差,演替初期的PF干、湿季"降温效应"分别为7.9%和3.6%,中期MF分别为11.6%和6.4%,顶级群落MEBF干、湿季"降温效应"可达15.7%和10.5%。总体上,随演替"降温增湿"效应越来越显著,且"降温"表现为干季更明显,而"增湿"表现为湿季明显。此外,演替驱动下后期森林对高温及土壤温度的调节作用更为突出。时间序列上,区域降水趋于"极端化"的格局影响下,森林生态系统的水分固持能力下降。主要表现为:自1984年以来,3种林型0—50cm土壤含水量均呈显著降低的趋势(P0.001),且湿季土壤含水量下降速率高于干季,林型间在全年及湿季均为MFMEBFPF,干季为MEBFMFPF。虽然研究期间3种林型林内气温、土壤温度无明显趋势性变化,但顶级群落MEBF林内相对湿度(P=0.021)、凋落物自然状态下含水量(P=0.003)在年际尺度上均呈现显著下降的趋势。与土壤含水量干、湿季下降速率的格局一致,二者也均为湿季大于干季。研究认为,成熟森林可能在当前南亚热带区域气候变化及水热格局改变背景影响下更为敏感和脆弱。     

Nitrogenase activity of two genotypes of Acacia mangium as affected by phosphorus nutrition

The specific nodulation, nitrogenase activity (acetylene reduction) and budgets of carbon allocation to respiration by nodulated roots were examined in two provenances of Acacia mangium Willd. grown in a glasshouse for 17 weeks to investigate the effects of soil phosphorus and genotypes of the host plant on symbiotic nitrogen fixation. Application of phosphorus (0–80 mg P kg^-1 soil) increased specific nodulation (g nodule dry weight g^-1 plant dry weight) of provenance Ma11 by two-fold and the percentage of nodulated root respiration allocated to nitrogenase by 50%, but had no effect on specific activity of nitrogenase or specific respiration coupled with nitrogenase activity. Improved phosphorus nutrition increased the specific nitrogenase activity of provenance Ma9 by 2-fold, the percentage of nodulated root respiration allocated to nitrogenase, and specific nitrogenase-linked respiration by 50%, respectively, but had no effect on the specific nodulation. The percentage of respiration coupled with nitrogenase activity in nodulated root respiration by provenance Ma9 was 60–70% higher than that in provenance Ma11, regardless of phosphorus levels applied. At the optimal level of phosphorus addition (10 mg P kg^-1 soil), provenance Ma9 had a lower dry mass than provenance Ma11. This was accompanied by a lower nodulated root respiration and a higher percentage of nodulated root respiration allocated to nitrogenase activity in provenance Ma9.     

Effects of elevated temperature on soil respiration in a coastal wetland during the non- growing season in the Yellow River Delta,China

Aims Winter soil respiration plays a crucial role in terrestrial carbon cycle, which could lose carbon gained in the growing season. With global warming, the average near-surface air temperatures will rise by 0.3 to 4.8 °C. Winter is expected to be warmer obviously than other seasons. Thus, the elevated temperature can significantly affect soil respiration. The coastal wetland has shallow underground water level and is affected by the fresh water and salt water. Elevated temperature can cause the increase of soil salinity, and as a result high salinity can limit soil respiration. Our objectives were to determine the diurnal and seasonal dynamics of soil respiration in a coastal wetland during the non-growing season, and to explore the responses of soil respiration to environmental factors, especially soil temperature and salinity.
Methods A manipulative warming experiment was conducted in a costal wetland in the Yellow River Delta using the infrared heaters. A complete random block design with two treatments, including control and warming, and each treatment was replicated each treatment four times. Soil respiration was measured twice a month during the non-growing season by a LI-8100 soil CO₂ efflux system. The measurements were taken every 2 h for 24 h at clear days. During each soil respiration measurement, soil environmental parameters were determined simultaneously, including soil temperature, moisture and salinity.
Important findings The diurnal variation of soil respiration in the warming plots was closely coupled with that in the control plots, and both exhibited single-peak curves. The daily soil respiration in the warming was higher than that in the control from November 2014 to January 2015. Contrarily, from March to April 2015. During the non-growing seasons, there were no significant differences in the daily mean soil respiration between the two treatments. However, soil temperature and soil salt content in the warming plots were significantly higher than those in the control plots. The non-growing season was divided into the no salt restriction period (November 2014 to middle February 2015) and salt restriction period (middle February 2015 to April 2015). During non-growing season, soil respiration in the warming had no significant difference compared with that in control. During the no salt restriction period, soil respiration in the warming was 22.9% (p < 0.01) greater than the control when soil temperature at 10 cm depth in warming was elevated by 4.0 °C compared with that in control. However, experimental warming decreased temperature sensitivity of soil respiration (Q₁₀). During salt restriction period, soil warming decreased soil respiration by 20.7% compared with the control although with higher temperature (3.3 °C), which may be attributed to the increased soil salt content (Soil electric conductivity increased from 4.4 ds·m^-1 to 5.3 ds·m^-1). The high water content can limit soil respiration in some extent. In addition, the Q₁₀ value in the warming had no significant difference compared with that in control during this period. Therefore, soil warming can not only increase soil respiration by elevating soil temperature, but also decrease soil respiration by increasing soil salt content due to evaporation, which consequently regulating the soil carbon balance of coastal wetlands.