土壤微生物膜对风沙土固沙保水特性的影响

土壤微生物膜胞外聚合物具有较强的黏结性,为增强风沙土抗蚀性,提高风沙土保水性提供了新途径。鉴于此,该研究采用室内控制试验设置6个微生物菌剂施用水平(0、1、3、5、7和10 g/kg),以期阐明土壤微生物膜对风沙土特性的影响。研究结果表明:1)施用微生物菌剂可产生土壤微生物膜,并胶结风沙土颗粒。2)试验结束时(第49 d),与对照组相比,不同菌剂施用处理的土壤容重降低0.54%～8.88%,孔隙度提高0.39%～3.91%,含水率显著提高0.11%～0.25%(P0.05),大团聚体质量分数增加5.59%～25.01%,土壤pH值由7.16显著增加至8.32～9.23(P0.05)。3)土壤多糖含量对土壤特性的解释率为47%,是影响土壤特性的关键因素。土壤微生物膜能够有效改善风沙土特性,增强风沙土抗蚀性,提高风沙土保水性,但较高的微生物菌剂施用量会增加土壤pH值,造成土壤盐碱化,建议微生物菌剂施用水平为1～5 g/kg。研究成果有利于深入理解微生物膜固沙保水机制,并可为沙化土地防治新技术研发提供重要理论依据和科技支撑。     

东北地区春玉米临界氮浓度稀释曲线的建立和验证

过量施氮是目前玉米栽培中存在的普遍现象,基于临界氮浓度稀释曲线计算得出的氮营养指数是诊断氮营养丰缺的重要手段。基于东北地区4个生态点的试验数据,构建了东北地区春玉米临界氮稀释曲线,并在此基础上建立了氮营养指数模型和需氮量模型,结果表明,东北地区春玉米地上部临界氮浓度与生物量符合幂函数关系。利用独立试验资料对建立的临界氮浓度稀释曲线进行检验,发现基于临界氮浓度稀释模型计算的氮营养指数可以准确诊断玉米植株的氮营养状况,并计算出实时的氮素需求量。该研究建立的东北地区春玉米临界氮稀释模型可以为该地区春玉米的氮营养诊断和动态调控提供较好的理论和技术指导。     

应用Excel软件分析敌敌畏农药对两广二号家蚕的安全间隔期

应用Excel软件中的曲线方程分析判断敌敌畏农药对两广二号家蚕的安全间隔期。结果表明：敌敌畏1000倍液的安全间隔期是6d多，其数学模型为幂函数曲线方：y=88．0653x-1834本方法克服以往家蚕的农药安全期无数学模型可循或使用的BASIC方法陈旧繁杂的缺点，也避免英文统计软件SPSS难以在农村普及的不足，是一种计...     

盐胁迫对裸果木幼苗光合特性的影响

本研究以一年生裸果木幼苗为材料，采用盆栽育苗方式，设计7个不同浓度NaCl溶液（CK、0.2%、0.4%、0.6%、0.8%、1.0% 和1.2%）模拟盐分胁迫，测定分析了其叶片气体交换参数、光响应曲线及叶绿素荧光参数的变化规律。结果表明：随着盐浓度的增加，叶片净光合速率（P_n）、气孔导度（G_s）和蒸腾速率（T_r）均呈下降趋势，NaCl浓度≥0.4%时，各处理P_n、G_s和T_r均显著低于CK；气孔限制值（L_s）和瞬时水分利用效率（WUE）随盐浓度增加呈先升后降趋势，胞间CO₂浓度（C_i）呈相反趋势，NaCl浓度为0.4%时，L_s达到最大值，而C_i达到最小值，说明P_n下降以气孔限制因素为主，而当NaCl浓度≥0.6%时，以非气孔限制为主要因素。随着盐胁迫程度的增大，最大净光合速率（P_nmax）、暗呼吸速率（R_d）、光饱和点（L_SP）、表观量子效率（A_QY）逐渐降低，光补偿点（L_CP）逐渐增加，表明盐分抑制了幼苗对光的吸收、利用和转换能力。叶片PSII潜在活性（F_v/F₀）、原初光能转化效率（F_v/F_m）、实际光化学效率（Φ_PSII）、电子传递速率（ETR）和光化学猝灭系数（q_p）随着盐浓度的增加呈下降趋势；非光化学猝灭系数（NPQ）在≤0.4%NaCl处理下较CK显著增加，盐浓度≥0.8%时，NPQ显著下降。基质的NaCl浓度在0.2%和0.4%时，裸果木叶片P_n、F_v/F₀、F_v/F_m下降不显著，WUE有所提高，PSII系统可以通过耗散过剩的光能保护光合机构，表现出一定的耐盐性；但盐浓度超过0.6%时，光合生态幅变窄，光合机构受到明显破坏，显著抑制了光合作用能力。     

风力发电场进场道路曲线设计应注意的问题

风能已成为世界上增长最快的清洁可再生能源,风力发电世界各国争相发展.然而我省风力发电项目进展较为缓慢,主要原因在于,我省公路网密度较低,许多公路等级偏低,平面线性较差,运输风电设备的长货车通行较困难.风电路的设计有一定的特殊性,我们在进行风电路设计时不能照搬规范上的数据,特殊数值需要通过计算求得,以保证风电设备的顺利运输.     

Temporal changes of soil physical quality under two residue management systems

Although crop residue management is known to affect near‐surface soil physical quality, little is known about the temporal variability of these indicators over short time intervals. This study evaluates the temporal changes of nine indicators of soil physical quality. These are organic carbon content, structural stability index, bulk density, macroporosity, air capacity, relative field capacity, plant available water capacity, Dexter's S‐index and saturated hydraulic conductivity. A second set of soil physical indicators, based on the distribution of soil pore volume, was also evaluated. The indicators were determined in three different times during the growing cycle of winter durum wheat cultivated within a long‐term field research carrying out in Southern Italy and comparing two types of crop residue management, that is, burning (B) and soil incorporation (I). Only the bulk density changed over time for both treatments, although the air capacity also changed for the incorporation of wheat residues. Residual effects of the autumnal soil tillage and soil compaction were a common source of variability, irrespective of which treatment was used. Based on the existing guidelines for evaluating the physical quality of these agricultural soils, optimal or near‐optimal values were detected in about half of the cases under consideration. This suggests that both B and I create sufficiently good conditions for crop growth during the crop cycle. The comparison between observed and optimal soil pore distribution function was always poor. The pore volume distributions showed lower densities of small pores and relatively higher densities of large pores than the proposed optimal distribution. This study also suggests that the considered optimal or references curves probably cannot be applied successfully to a wide range of agricultural soils.     

SoilFlex‐LLWR: linking a soil compaction model with the least limiting water range concept

Soil compaction impacts growing conditions for plants: it increases the mechanical resistance to root growth and modifies the soil pore system and consequently the supply of water and oxygen to the roots. The least limiting water range (LLWR) defines a range of soil water contents within which root growth is minimally limited with regard to water supply, aeration and penetration resistance. The LLWR is a function of soil bulk density (BD), and hence directly affected by soil compaction. In this paper, we present a new model, ‘SoilFlex‐LLWR’, which combines a soil compaction model with the LLWR concept. We simulated the changes in LLWR due to wheeling with a self‐propelled forage harvester on a Swiss clay loam soil (Gleyic Cambisol) using the new SoilFlex‐LLWR model, and compared measurements of the LLWR components as a function of BD with model estimations. SoilFlex‐LLWR allows for predictions of changes in LLWR due to compaction caused by agricultural field traffic and therefore provides a quantitative link between impact of soil loading and soil physical conditions for root growth.     

Impacts of population growth, economic development, and technical change on global food production and consumption

Over the next decades mankind will demand more food from fewer land and water resources. This study quantifies the food production impacts of four alternative development scenarios from the Millennium Ecosystem Assessment and the Special Report on Emission Scenarios. Partially and jointly considered are land and water supply impacts from population growth, and technical change, as well as forest and agricultural commodity demand shifts from population growth and economic development. The income impacts on food demand are computed with dynamic elasticities. Simulations with a global, partial equilibrium model of the agricultural and forest sectors show that per capita food levels increase in all examined development scenarios with minor impacts on food prices. Global agricultural land increases by up to 14% between 2010 and 2030. Deforestation restrictions strongly impact the price of land and water resources but have little consequences for the global level of food production and food prices. While projected income changes have the highest partial impact on per capita food consumption levels, population growth leads to the highest increase in total food production. The impact of technical change is amplified or mitigated by adaptations of land management intensities.     

Hydro-physical responses of gypseous and non-gypseous soils to livestock grazing in a semi-arid region of NE Spain

Pasture productivity depends on soil hydro-physical properties, which in turn are deeply affected by livestock grazing. However, the comparative response of different soil types, and particularly gypseous soil types, to grazing has hardly been studied before. This paper compares the effect of grazing on the soil hydro-physical properties of silty gypseous (Gy) and non-gypseous (NGy) soils located in a semi-arid region (Middle Ebro Valley, NE, Spain). Two different soil managements were selected: ungrazed natural shrubland (N) and grazed shrubland (GR) soils. The gypsum, CaCO₃ and organic matter content (OM), soil texture, soil bulk density (ρ_b), penetration resistance (PR), saturated sorptivity (S), hydraulic conductivity (K), and the water retention curve (WRC) for undisturbed soil samples from 1 to 10 cm depth soil layer were measured. The ρ_b and PR in NGy soils were significantly higher than those observed in the Gy ones. Soil compaction due to grazing treatment tended to increase ρ_b and decrease the K and S values. While no differences in PR were observed in the Gy soils between grazing treatments, the PR measured in the NGy soils under GR was significantly higher than the corresponding values observed under N. Differences in K and S between GR and N treatments were only significant (p < 0.05) in NGy soils, where K and S values under the N treatment were almost four times greater than the corresponding values measured under GR. Overall, no differences in the WRCs were observed between soil types and grazing treatments. While the WRCs of NGy soils were not significantly affected by the grazing treatment, Gy soils under N treatment present a significantly higher level of soil macropores than under GR treatment. The hydro-physical features of Gy soils tended to be less affected by grazing than those of the NGy soils. These results suggest that livestock grazing, in both Gy and NGy soils, has a negative effect on the physical soil properties, which should be taken into account by land managers of these semi-arid regions where silty gypseous and non-gypseous areas coexist.     

Origin软件在研究市售滴灌产品水力性能中的应用

滴灌是一种受到广泛关注的低压节水灌溉技术,滴灌产品作为承栽该技术的载体,其质量直接影响了滴灌技术的推广。通常那些制造偏差小、流量均匀度高、抗堵塞性能强、单位成本低的滴灌产品才能得到更广泛的应用。采用最小二乘法,使用origin软件对市售的4种主要滴灌产品压力一流量关系进行拟合计算,结果表明：使用该软件拟合的流量及水利性...