CO_2,CH_4 and N_2O flux changes in degraded grassland soil of Inner Mongolia,China

The main purpose of this study was to explore the dynamic changes of greenhouse gas(GHG)from grasslands under different degradation levels during the growing seasons of Inner Mongolia, China.Grassland degradation is associated with the dynamics of GHG fluxes, e.g., CO_2, CH_4 and N_2O fluxes. As one of the global ecological environmental problems, grassland degradation has changed the vegetation productivity as well as the accumulation and decomposition rates of soil organic matter and thus will influence the carbon and nitrogen cycles of ecosystems, which will affect the GHG fluxes between grassland ecosystems and the atmosphere. Therefore, it is necessary to explore how the exchanges of CO_2,CH_4 and N_2O fluxes between soil and atmosphere are influenced by the grassland degradation. We measured the fluxes of CO_2, CH_4 and N_2O in lightly degraded, moderately degraded and severely degraded grasslands in Inner Mongolia of China during the growing seasons from July to September in 2013 and 2014. The typical semi-arid grassland of Inner Mongolia plays a role as the source of atmospheric CO_2 and N_2O and the sink for CH_4. Compared with CO_2 fluxes, N_2O and CH_4 fluxes were relatively low. The exchange of CO_2, N_2O and CH_4 fluxes between the grassland soil and the atmosphere may exclusively depend on the net exchange rate of CO_2 in semi-arid grasslands. The greenhouse gases showed a clear seasonal pattern, with the CO_2 fluxes of –33.63–386.36 mg/(m·h), CH_4 uptake fluxes of 0.113–0.023 mg/(m·h) and N_2O fluxes of –1.68–19.90 μg/(m·h). Grassland degradation significantly influenced CH_4 uptake but had no significant influence on CO_2 and N_2O emissions. Soil moisture and temperature were positively correlated with CO_2 emissions but had no significant effect on N_2O fluxes.Soil moisture may be the primary driving factor for CH_4 uptake. The research results can be in help to better understand the impact of grassland degradation on the ecological environment.     

Grazing alters sandy soil greenhouse gas emissions in a sand-binding area of the Hobq Desert,China

Deserts are sensitive to environmental changes caused by human interference and are prone to degradation. Revegetation can promote the reversal of desertification and the subsequent formation of fixed sand. However, the effects of grazing, which can cause the ground-surface conditions of fixed sand to further deteriorate and result in re-desertification, on the greenhouse gas (GHG) fluxes from soils remain unknown. Herein, we investigated GHG fluxes in the Hobq Desert, Inner Mongolia Autonomous Region of China, at the mobile (desertified), fixed (vegetated), and grazed (re-desertified) sites from January 2018 to December 2019. We analyzed the response mechanism of GHG fluxes to micrometeorological factors and the variation in global warming potential (GWP). CO₂ was emitted at an average rate of 4.2, 3.7, and 1.1 mmol/(m²•h) and N₂O was emitted at an average rate of 0.19, 0.15, and 0.09 µmol/(m²•h) at the grazed, fixed, and mobile sites, respectively. Mean CH₄ consumption was as follows: fixed site (2.9 µmol/(m²•h))>grazed site (2.7 µmol/(m²•h))>mobile site (1.1 µmol/(m²•h)). GHG fluxes varied seasonally, and soil temperature (10 cm) and soil water content (30 cm) were the key micrometeorological factors affecting the fluxes. The changes in the plant and soil characteristics caused by grazing resulted in increased soil CO₂ and N₂O emissions and decreased CH₄ absorption. Grazing also significantly increased the GWP of the soil (P<0.05). This study demonstrates that grazing on revegetated sandy soil can cause re-desertification and significantly increase soil carbon and nitrogen leakage. These findings could be used to formulate informed policies on the management and utilization of desert ecosystems.     

温性荒漠草地蒿类半灌木合理需水量探讨

文中对新疆伊犁河流域温性荒漠草地蒿类半灌木生物量随水分条件的变化规律进行了研究。结果显示:随着灌溉水量的增加,单位面积蒿类生物量明显表现出先增加然后下降的变化规律。据灵敏度(Sk)计算,灌溉水量在433kg/(m2.a)时,Sk存在最大值,表明此时地表生物量对灌溉水量变化的响应最为灵敏。根据灵敏度变化曲线将不同灌溉水量下地表生物量变化分为3个区间。灌溉水量在(226kg/(m2.a)—778kg/(m2.a))区间,蒿类生物量增加的幅度超过灌溉水量变化的幅度,实施此灌溉水量可得到最优恢复效果。因此恢复当地草地的合理水量范围确定在(226kg/(m2.a)—778kg/(m2.a))。从水资源利用的效率看,选择228kg/(m2.a)作为蒿类荒漠草地恢复的最小需水量更为合理。     

Fluxes of methane,carbon dioxide and nitrous oxide in an alpine wetland and an alpine grassland of the Tianshan Mountains,China

Methane(CH4), carbon dioxide(CO2) and nitrous oxide(N2O) are known to be major greenhouse gases that contribute to global warming. To identify the flux dynamics of these greenhouse gases is, therefore, of great significance. In this paper, we conducted a comparative study on an alpine grassland and alpine wetland at the Bayinbuluk Grassland Eco-system Research Station, Chinese Academy of Sciences. By using opaque, static, manual stainless steel chambers and gas chromatography, we measured the fluxes of CH4, N2O and CO2 from the grassland and wetland through an in situ monitoring study from May 2010 to October 2012. The mean flux rates of CH4, N2O and CO2 for the experimental alpine wetland in the growing season(from May to October) were estimated at 322.4 μg/(m2?h), 16.7 μg/(m2?h) and 76.7 mg/(m2?h), respectively; and the values for the alpine grassland were –88.2 μg/(m2?h), 12.7 μg/(m2?h), 57.3 mg/(m2?h), respectively. The gas fluxes showed large seasonal and annual variations, suggesting weak fluxes in the non-growing season. The relationships between these gas fluxes and environmental factors were analyzed for the two alpine ecosystems. The results showed that air temperature, precipitation, soil temperature and soil moisture can greatly influence the fluxes of CH4, N2O and CO2, but the alpine grassland and alpine wetland showed different feedback mechanisms under the same climate and environmental conditions.     

Carbon storage in a wolfberry plantation chronosequence established on a secondary saline land in an arid irrigated area of Gansu Province,China

Carbon(C) storage has received significant attention for its relevance to agricultural security and climate change. Afforestation can increase C storage in terrestrial ecosystems, and has been recognized as an important measure to offset CO_2 emissions. In order to analyze the C benefits of planting wolfberry(Lycium barbarum L.) on the secondary saline lands in arid areas, we conducted a case study on the dynamics of biomass carbon(BC) storage and soil organic carbon(SOC) storage in different-aged wolfberry plantations(4-, 7-and 11-year-old) established on a secondary saline land as well as on the influence of wolfberry plantations on C storage in the plant-soil system in an arid irrigated area(Jingtai County) of Gansu Province, China. The C sequestration and its potential in the wolfberry plantations of Gansu Province were also evaluated. An intact secondary saline land was selected as control. Results show that wolfberry planting could decrease soil salinity, and increase BC, SOC and litter C storage of the secondary saline land significantly, especially in the first 4 years after planting. The aboveground and belowground BC storage values in the intact secondary saline land(control) accounted for only 1.0% and 1.2% of those in the wolfberry plantations, respectively. Compared to the intact secondary saline land, the SOC storage values in the 4-, 7-and 11-year-old wolfberry plantations increased by 36.4%, 37.3% and 43.3%, respectively, and the SOC storage in the wolfberry plantations occupied more than 92% of the ecosystem C storage. The average BC and SOC sequestration rates of the wolfberry plantations for the age group of 0–11 years were 0.73 and 3.30 Mg C/(hm~2·a), respectively. There were no significant difference in BC and SOC storage between the 7-year-old and 11-year-old wolfberry plantations, which may be due in part to the large amounts of C offtakes in new branches and fruits. In Gansu Province, the C storage in the wolfberry plantations has reached up to 3.574 Tg in 2013, and the C sequestration potential of the existing wolfberry plantations was 0.134 Tg C/a. These results indicate that wolfberry planting is an ideal agricultural model to restore the degraded saline lands and increase the C sequestration capacity of agricultural lands in arid areas.     

Response of soil N_2O emissions to precipitation pulses under different nitrogen availabilities in a semiarid temperate steppe of Inner Mongolia,China

Short-term nitrous oxide（N2O） pulse emissions caused by precipitation account for a considerable portion of the annual N2O emissions and are greatly influenced by soil nitrogen（N） dynamics. However, in Chinese semiarid temperate steppes, the response of N2O emissions to the coupling changes of precipitation and soil N availability is not yet fully understood. In this study, we conducted two 7-day field experiments in a semiarid temperate typical steppe of Inner Mongolia, China, to investigate the N2O emission pulses resulting from artificial precipitation events（approximately equivalent to 10.0 mm rainfall） under four N addition levels（0, 5, 10 and 20 g N/（m2·a）） using the static opaque chamber technique. The results show that the simulated rainfall during the dry period in 2010 caused greater short-term emission bursts than that during the relatively rainy observation period in 2011（P〈0.05）. No significant increase was observed for either the N2O peak effluxes or the weekly cumulative emissions（P〉0.05） with single water addition. The peak values of N2O efflux increased with the increasing N input. Only the treatments with water and medium（WN10） or high N addition（WN20） significantly increased the cumulative N2O emissions（P〈0.01） in both experimental periods. Under drought condition, the variations in soil N2O effluxes were positively correlated with the soil NH4-N concentrations in the three N input treatments（WN5, WN10, and WN20）. Besides, the soil moisture and temperature also greatly influenced the N2O pulse emissions, particularly the N2O pulse under the relatively rainy soil condition or in the treatments without N addition（ZN and ZWN）. The responses of the plant metabolism to the varying precipitation distribution and the length of drought period prior to rainfall could greatly affect the soil N dynamics and N2O emission pulses in semiarid grasslands.     

甘肃糜子(Panicum miliaceum L.)生态气候适宜性研究

为探讨糜子种植的生态气候适宜性,运用积分回归方法,对庆阳西峰区、天水麦积区、定西安定区及武威凉州区1985~2008年糜子产量受气候因子的影响进行了分析。结果表明:水热因子在不同的生育阶段对不同地点糜子的产量影响各不相同;在抽穗~开花期间,旬平均气温对安定、凉州、西峰、麦积糜子产量影响较大,分别为10.5 kg/(hm2.℃)9、.0 kg/(hm2.℃)8、.0 kg/(hm2.℃)及5.6 kg/(hm2.℃),在拔节期旬降水量对产量影响较大,分别为8.0 kg/(hm2.mm)3、.0 kg/(hm2.mm)5、.2 kg/(hm2.mm)及5.2 kg/(hm2.mm);甘肃各地光照基本上都能满足糜子的生长发育需要;最适宜种植区为陇东的塬区、渭河谷地及河西海拔在1 600 m以下灌溉区及敦煌盆地;最具有潜力的种植区为陇中地区及陇东的北部。     

Effects of Caragana microphylla plantations on organic carbon sequestration in total and labile soil organic carbon fractions in the Horqin Sandy Land,northern China

Afforestation is conducive to soil carbon(C) sequestration in semi-arid regions. However, little is known about the effects of afforestation on sequestrations of total and labile soil organic carbon(SOC) fractions in semi-arid sandy lands. In the present study, we examined the effects of Caragana microphylla Lam. plantations with different ages(12-and 25-year-old) on sequestrations of total SOC as well as labile SOC fractions such as light fraction organic carbon(LFOC) and microbial biomass carbon(MBC). The analyzed samples were taken from soil depths of 0–5 and 5–15 cm under two shrub-related scenarios: under shrubs and between shrubs with moving sand dunes as control sites in the Horqin Sandy Land of northern China. The results showed that the concentrations and storages of total SOC at soil depths of 0–5 and 5–15 cm were higher in 12-and 25-year-old C. microphylla plantations than in moving sand dunes(i.e., control sites), with the highest value observed under shrubs in 25-year-old C. microphylla plantations. Furthermore, the concentrations and storages of LFOC and MBC showed similar patterns with those of total SOC at the same soil depth. The 12-year-old C. microphylla plantations had higher percentages of LFOC concentration to SOC concentration and MBC concentration to SOC concentration than the 25-year-old C. microphylla plantations and moving sand dunes at both soil depths. A significant positive correlation existed among SOC, LFOC, and MBC, implying that restoring the total and labile SOC fractions is possible by afforestation with C. microphylla shrubs in the Horqin Sandy Land. At soil depth of 0–15 cm, the accumulation rate of total SOC under shrubs was higher in young C. microphylla plantations(18.53 g C/(m~2·a); 0–12 years) than in old C. microphylla plantations(16.24 g C/(m~2·a); 12–25 years), and the accumulation rates of LFOC and MBC under shrubs and between shrubs were also higher in young C. microphylla plantations than in old C. microphylla plantations. It can be concluded that the establishment of C. microphylla in the Horqin Sandy Land may be a good mitigation strategy for SOC sequestration in the surface soils.     

Influences of drip and flood irrigation on soil carbon dioxide emission and soil carbon sequestration of maize cropland in the North China Plain

The need is pressing to investigate soil CO_2(carbon dioxide) emissions and soil organic carbon dynamics under water-saving irrigation practices in agricultural systems for exploring the potentials of soil carbon sequestration. A field experiment was conducted to compare the influences of drip irrigation(DI) and flood irrigation(FI) on soil organic carbon dynamics and the spatial and temporal variations in CO_2 emissions during the summer maize growing season in the North China Plain using the static closed chamber method. The mean CO_2 efflux over the growing season was larger under DI than that under FI. The cumulative CO_2 emissions at the field scale were 1959.10 and 1759.12 g/m~2 under DI and FI, respectively. The cumulative CO_2 emission on plant rows(OR) was larger than that between plant rows(BR) under FI, and the cumulative CO2 emission on the irrigation pipes(OP) was larger than that between irrigation pipes(BP) under DI. The cumulative CO_2 emissions of OP, BP and bare area(BA) under DI were larger than those of OR, BR and BA under FI, respectively. Additionally, DI promoted root respiration more effectively than FI did. The average proportion of root respiration contributing to the soil CO_2 emissions of OP under DI was larger than that of OR under FI. A general conclusion drawn from this study is that soil CO_2 emission was significantly influenced by the soil water content, soil temperature and air temperature under both DI and FI. Larger concentrations of dissolved organic carbon(DOC), microbial biomass carbon(MBC) and total organic carbon(TOC) were observed under FI than those under DI. The observed high concentrations(DOC, MBC, and TOC) under FI might be resulted from the irrigation-associated soil saturation that in turn inhibited microbial activity and lowered decomposition rate of soil organic matter. However, DI increased the soil organic matter quality(the ratio of MBC to TOC) at the depth of 10–20 cm compared with FI. Our results suggest that the transformation from conventional FI to integrated DI can increase the CO2 emissions and DI needs to be combined with other management practices to reduce the CO_2 emissions from summer maize fields in the North China Plain.     

Wind tunnel experiments on dust emissions from different landform types

The measurement and assessment of dust emissions from different landforms are important to understand the atmospheric loading of PM10(particulate matter ≤10 μm aerodynamic diameter) and to assess natural sources of dust; however, the methodology and technique for determining the dust still present significant research challenges. In the past, specialized field observation and field wind tunnel studies have been used to understand the dust emission. A series of wind tunnel tests were carried out to identify natural sources of dust and measure the magnitudes of dust emissions from different landforms. The method used in this study allowed the measurement of the PM10 emission rate using a laboratory based environmental boundary layer wind tunnel. Results indicated that PM10 emissions demonstrated strong temporal variation and were primarily driven by aerodynamic entrainment. Sand dunes, playa, and alluvial fans had the largest dust emission rates(0.8–5.4 mg/(m~2·s)) while sandy gravel, Gobi desert and abandoned lands had the lowest emission rates(0.003–0.126 mg/(m~2·s)). Dust emissions were heavily dependent on the surface conditions, especially the availability of loose surface dust. High dust emissions were a result of the availability of dustparticle materials for entrainment while low dust emissions were a result of surface crusts and gravel cover. Soil surface property(surface crusts and gravel cover) plays an important role in controlling the availability of dust-sized particles for entrainment. The dust emission rate depended not only on the surface conditions but also on the friction velocity. The emission rate of PM10 varies as a power function of the friction velocity. Although dynamic abrasion processes have a strong influence on the amount of dust entrainment, aerodynamic entrainment may provide an important mechanism for dust emissions. Large volumes of dust entrained by aerodynamic entrainment cannot only occur at low shear velocity without saltation, but may dominate the entrainment process in many arid and semi-arid environments. So it may also be responsible for large magnitude dust storms. Playa and alluvial fan landforms, prior to developing a surface crust, may be the main sources of dust storms in Qinghai Province.     

Carbon fixation and influencing factors of biological soil crusts in a revegetated area of the Tengger Desert,northern China

Biological soil crusts （BSCs） are an important type of land cover in arid desert landscapes and play an important role in the carbon source-sink exchange within a desert system. In this study, two typical BSCs, moss crusts and algae crusts, were selected from a revegetated sandy area of the Tengger Desert in northern China, and the experiment was carried out over a 3-year period from January 2010 to November 2012. We obtained the effec- tive active wetting time to maintain the physiological activity of BSCs basing on continuous field measurements and previous laboratory studies on BSCs photosynthesis and respiration rates. And then we developed a BSCs carbon fixation model that is driven by soil moisture. The results indicated that moss crusts and algae crusts had significant effects on soil moisture and temperature dynamics by decreasing rainfall infiltration. The mean carbon fixation rates of moss and algae crusts were 0.21 and 0.13 g C/（m2.d）, respectively. The annual carbon fixations of moss crusts and algae crusts were 64.9 and 38.6 g C/（m2.a）, respectively, and the carbon fixation of non-rainfall water reached 11.6 g C/（m2.a） （30.2% of the total） and 8.8 g C/（m2.a） （43.6% of the total）, respectively. Finally, the model was tested and verified with continuous field observations. The data of the modeled and measured CO2 fluxes matched notably well. In desert regions, the carbon fixation is higher with high-frequency rainfall even the total amount of seasonal rainfall was the same.     

24%丙硫 ? 戊唑醇悬浮剂的研制及其对稻麦纹枯病的防治效果

丙硫菌唑是一种新型广谱三唑硫酮类杀菌剂。通过联合效力 (联合毒力) 测定、配方助剂筛选和悬浮剂理化性能指标检测,研制了丙硫菌唑与戊唑醇复配的悬浮剂,并测定了其对水稻、小麦纹枯病的防治效果。结果表明:丙硫菌唑与戊唑醇质量比为2 : 1时对稻麦纹枯病菌具有增效作用,联合效力系数 (共毒系数) 分别为1.91和1.92;24%丙硫 ? 戊唑醇悬浮剂最佳配方 (质量分数) 为:16.0%丙硫菌唑、8.0%戊唑醇、4.0% 分散剂Featdis SCP、3.0% 润湿剂EFW、0.2%黄原胶、1.0%硅酸镁铝和4%乙二醇,水补足至100%。产品经过(54 ± 2) ℃热贮14 d后,悬浮率95.2%,pH值6.9,平均粒径0.71 μm,析水率2.3%,持久起泡性小于25 mL;(0 ± 2) ℃冷贮7 d后,悬浮率94.8%,pH值7.1,平均粒径0.87 μm,持久起泡性小于25 mL,黏度在200~600 mPa·s之间。田间防效测定结果表明,24%丙硫 ? 戊唑醇悬浮剂对水稻、小麦纹枯病均有较好防效,田间施用量 (有效成分) 210 g/hm2和150 g/hm2时,防效分别达89.01%和86.26%。     

秸秆还田对半干旱区农田土壤养分含量及玉米光合作用的影响

为了提升和保育辽西半干旱区农田土壤质量,采用盆栽试验的方式探讨了不同处理方式、不同用量玉米秸秆还田对土壤养分含量的影响。结果表明,秸秆还田后,其土壤含水量比对照组提高了3%~7%;有机质含量比对照组提高幅度为1.9%~19%;全氮含量比对照组提高幅度为0.7%~14.4%;速效磷含量比对照组提高了2.51~14.75 mg/kg;速效钾含量比对照组提高了7.33~188.07 mg/kg;碱解氮含量比对照组提高了8.46mg/kg;净光合速率比对照组提高了3~11.03 CO2μmol/(m2.s);秸秆还田可以缓解土壤碱化。     

Effects of disease control by fungicides on greenhouse gas emissions by UK arable crop production

BACKGROUND: The UK government has published plans to reduce UK agriculture's greenhouse gas (GHG) emissions. At the same time, the goal of global food security requires an increase in arable crop yields. Foliar disease control measures such as fungicides have an important role in meeting both objectives. RESULTS: It is estimated that UK winter barley production is associated with GHG emissions of 2770 kg CO₂ eq. ha^?1 of crop and 355 kg CO₂ eq. t^?1 of grain. Foliar disease control by fungicides is associated with decreases in GHG emissions of 42–60 kg CO₂ eq. t^?1 in UK winter barley and 29–39 kg CO₂ eq. t^?1 in UK spring barley. The sensitivity of these results to the impact of disease control on yield and to variant GHG emissions assumptions is presented. Fungicide treatment of the major UK arable crops is estimated to have directly decreased UK GHG emissions by over 1.5 Mt CO₂ eq. in 2009. CONCLUSION: Crop disease control measures such as fungicide treatment reduce the GHG emissions associated with producing a tonne of grain. As national demand for food increases, greater yields as a result of disease control also decrease the need to convert land from non‐arable to arable use, which further mitigates GHG emissions. Copyright © 2011 Society of Chemical Industry     

长武塬区光合有效辐射的基本特征及气候学计算

利用长武农业生态试验站2010年气象观测资料,分析了长武塬区光合有效辐射及其占太阳总辐射比例系数的日变化、季节变化特征和影响因素。结果表明:就日变化过程而言,光合有效辐射和总辐射趋势一致,晴天呈单峰型,起伏平滑;阴天的形状则不稳定,最大值出现在12∶30~15∶00之间。光合有效辐射具有明显的季节变化特征,春夏较大,秋季次之,冬季最小,从春到冬其平均日总量分别为6.32、7.23、5.63MJ/m2和3.58MJ/m2。光合有效辐射系数阴天大,晴天小;就月平均值而论,6月份最大,为0.423,1月份最小,为0.327。根据观测数据,论文给出了适合该地区的光合有效辐射计算的经验模型。     

利用凝胶扩散法测定刺萼龙葵种子中β-甘露聚糖酶的活性

β-甘露聚糖酶是种子萌发过程中降解胚乳细胞壁的关键酶,明确其活性的动态变化可为揭示杂草种子的休眠萌发机制提供重要依据。以外来杂草刺萼龙葵Solanum rostratum Dunal种子为材料,建立了种子中β-甘露聚糖酶活性的检测方法—凝胶扩散法。利用凝胶扩散法对不同贮存时间及贮存条件下刺萼龙葵种子中β-甘露聚糖酶的活性进行了检测,发现贮存3年以上的种子中该酶的活性为0.03 nmol/(min·mg),显著低于贮存3年以下的种子中的酶活性0.15 nmol/(min·mg),而湿润冷藏的种子中β-甘露聚糖酶的活性为0.12 nmol/(min·mg),显著高于干燥冷藏的种子的酶活性0.02 nmol/(min·mg)。实际应用结果表明,凝胶扩散法综合了传统方法的优势,检测特异性强、灵敏度高、重复性好,可同时检测大量种子样品,具有良好的实用性。     

双垄全膜覆盖沟播栽培对甘肃中部坡耕地水土流失和作物产量的影响

在甘肃省榆中县黄土高原丘陵沟壑区的坡耕地,采用双垄全膜覆盖沟播(DRM)、全膜平铺覆盖(WM)、条膜(半膜)起垄覆盖(RM)、条膜(半膜)平铺覆盖(NM)、露地条播(CK)5个处理进行对比试验。结果表明,双垄全膜覆盖沟播栽培具有良好的减少坡耕地土壤水土流失的作用,土壤流失量分别较露地条播、条膜起垄、条膜平铺、全膜平铺下降了56.07%、67.24%、71.59%、82.47%;作物产量大幅度提高,玉米产量分别比半膜垄作和半膜平铺增产46.76%和58.07%,蚕豆产量分别比条膜起垄、条膜平铺和对照增产46.52%、54.99%和102.96%,马铃薯产量分别比条膜起垄、条膜平铺和对照增产95.21%、76.30%和74.89%。玉米的水分生产率分别比半膜垄作和半膜平铺提高4.77 kg/(mm.hm2)和9.47 kg/(mm.hm2),蚕豆的水分生产率比半膜垄作、半膜平铺和露地对照提高3.24、6.58 kg/(mm.hm2)和5.03 kg/(mm.hm2),马铃薯的水分生产率比半膜垄作、半膜平铺和露地对照提高47.35、42.02、41.57 kg/(mm.hm2)。黄土高原丘陵沟壑半干旱雨养农业区坡耕地采用双垄全膜覆盖沟播栽培,具有良好的减少土壤水土流失的作用,能够最大限度地集蓄天然降水,加之其明显的增温保温作用,可大幅度地提高作物产量,降水生产率显著提高。     

Gross nitrogen transformations and N_2O emission sources in sandy loam and silt loam soils

The soil type is a key factor influencing N(nitrogen) cycling in soil; however, gross N transformations and N_2O emission sources are still poorly understood. In this study, a laboratory ~(15)N tracing experiment was carried out at 60% WHC(water holding capacity) and 25℃ to evaluate the gross N transformation rates and N_2O emission pathways in sandy loam and silt loam soils in a semi-arid region of Heilongjiang Province, China. The results showed that the gross rates of N mineralization, immobilization, and nitrification were 3.60, 1.90, and 5.63 mg N/(kg·d) in silt loam soil, respectively, which were 3.62, 4.26, and 3.13 times those in sandy loam soil, respectively. The ratios of the gross nitrification rate to the ammonium immobilization rate(n/ia) in sandy loam soil and silt loam soil were all higher than 1.00, whereas the n/ia in sandy loam soil(4.36) was significantly higher than that in silt loam soil(3.08). This result indicated that the ability of sandy loam soil to release and conserve the available N was relatively poor in comparison with silt loam soil, and the relatively strong nitrification rate compared to the immobilization rate may lead to N loss through NO_3~– leaching. Under aerobic conditions, both nitrification and denitrification made contributions to N_2O emissions. Nitrification was the dominant pathway leading to N_2O production in soils and was responsible for 82.0% of the total emitted N_2O in sandy loam soil, which was significantly higher than that in silt loam soil(71.7%). However, the average contribution of denitrification to total N_2O production in sandy loam soil was 17.9%, which was significantly lower than that in silt loam soil(28.3%). These results are valuable for developing reasonable fertilization management and proposing effective greenhouse gas mitigation strategies in different soil types in semiarid regions.     

综合改培措施对樟树成龄低质林生长、 材积和经济效益的影响

[目的]为明确抚育间伐和施肥综合改培技术措施对江西大岗山地区樟树成龄低质人工林生长、蓄积和经济效益的影响.[方法]课题组在安福县明月山林场泰山分场设置试验林,对樟树人工林实施综合改培措施与未采取经营措施的进行对照,分析效果效应.[结果]综合改培措施实施1年后,樟树径向生长量比对照提高了33.33％,单位面积蓄积生长量比...     

新疆玛纳斯河径流时间变化特征及其趋势分析

依据新疆玛纳斯河肯斯瓦特水文站近46年实测月径流量资料,采用Morlet小波分析,径流集中度、轮次分析、游程检验、极差分析、气候趋势系数法等方法分析了玛纳斯河径流系列多时间尺度变化特征及其未来变化趋势。结果表明:玛纳斯河年径流系列存在7年及25年主周期;极限枯水历时达8年,平均缺水4.40m3/s;单独丰水年概率高于单独枯水年概率,发生3年及以上连枯年概率均高于连丰年,易发生持续干旱;玛纳斯河年径流和夏季径流显著增加(P=0.01),幅度分别为2.24m3/(s·10a)及7.45m3/(s·10a),夏季径流增加尤为明显;秋季和冬季径流也呈现增加趋势(P=0.05),幅度分别为0.45m3/(s·10a)及0.49m3/(s·10a)。