不同水肥条件下夏玉米/冬小麦农田生态系统碳平衡研究

农田生态系统碳平衡取决于农作物固定碳量和土壤异养呼吸排放碳量。为揭示水肥用量对农田生态系统碳平衡的综合影响，设置3个灌水水平：高水、中水和低水（W1、W0.85、W0.7夏玉米季分别为90、76.5、63mm，冬小麦季分别为140、119、98mm），4个施氮水平：高氮、中氮、低氮和不施氮（N1、N0.85、N0.7、N0夏玉米季分别为300、255、210、0kg/hm2，冬小麦季分别为210、178.5、147、0kg/hm2），4个施磷水平：高磷、中磷、低磷和不施磷（P1、P0.85、P0.7和P0夏玉米季分别为90、76.5、63、0kg/hm2，冬小麦季分别为150、127.5、105、0kg/hm2）进行了田间试验。结果表明：不同水肥处理下夏玉米/冬小麦农田生态系统表现为碳汇，夏玉米季净生态系统生产力固碳量（CNEP）为6805~7233kg/hm2，冬小麦季CNEP为5842~6434kg/hm2，夏玉米CNEP高于冬小麦。在高、中、低肥水平下，增加灌水量，夏玉米/冬小麦周年净初级生产力固碳量（CNPP）提高2.48%~5.96%，土壤微生物异养呼吸碳释放量（CRm）增加2.15%~15.20%，净生态系统生产力固碳量（CNEP）增加1.16%~6.47%。在高、中、低供水水平下，增加施肥量，夏玉米/冬小麦周年CNPP增加2.95%~3.43%，土壤CRm增加5.23%~18.67%，CNEP增加0.93%~2.79%，CNEP增加比例与供水水平呈负相关。在低水条件下，氮磷肥配施处理夏玉米/冬小麦农田周年CNEP较单施氮、磷肥分别增加4.86%、7.34%，且氮磷肥交互作用显著（P<0.05），水肥供应水平相差15%时对冬小麦农田CNEP有显著的正交互作用。氮磷肥配施、水肥协调供应均有助于促进夏玉米/冬小麦农田生态系统的净碳输入，在节水节肥原则下，夏玉米和冬小麦分别在W0.85N0.85P0.85和W0.7N0.85P0.85水肥供应条件下有利于增加农田CNEP。     

Poorly crystalline iron and aluminium oxides contribute to the carbon saturation and sorption of dissolved organic carbon in the soil

Soil carbon (C) saturation implies an upper limit to a soil's capacity to store C depending on the contents of silt + clay and poorly crystalline Fe and Al oxides. We hypothesized that the poorly crystalline Fe and Al oxides in silt + clay fraction increased the C saturation and thus reduced the capacity of the soil to sorb additional C input. To test the hypothesis, we studied the sorption of dissolved organic carbon (DOC) on silt + clay fractions (<53 µm) of highly weathered oxic soils, collected from three different land uses (i.e., improved pasture, cropping and forest). Soils with high carbon saturation desorbed 38% more C than soils with low C saturation upon addition of DOC, whereas adsorption of DOC was only observed at higher concentration (>15 g kg^?1). While high Al oxide concentration significantly increased both the saturation and desorption of DOC, the high Fe oxide concentration significantly increased the desorption of DOC, supporting the proposition that both oxides have influence on the DOC sorption in soil. Our findings provide a new insight into the chemical control of stabilization and destabilization of DOC in soil.     

Effect of farm management on topsoil organic carbon and aggregate stability in water: A case study from Southwest England,UK

There are few reliable data sets to inspire confidence in policymakers that soil organic carbon (SOC) can be measured on farms. We worked with farmers in the Tamar Valley region of southwest England to select sampling sites under similar conditions (soil type, aspect and slope) and management types. Topsoils (2–15 cm) were sampled in autumn 2015, and percentage soil organic matter (%SOM) was determined by loss on ignition and used to calculate %SOC. We also used the stability of macroaggregates in cold water (WSA) (‘soil slaking’) as a measure of ‘soil health’ and investigated its relationship with SOC in the clay‐rich soils. %SOM was significantly different between management types in the order woodland (11.1%) = permanent pasture (9.5%) > ley‐arable rotation (7.7%) = arable (7.3%). This related directly to SOC stocks that were larger in fields under permanent pasture and woodland compared with those under arable or ley‐arable rotation whether corrected for clay content (F = 8.500, p < .0001) or not (F = 8.516, p < .0001). WSA scores were strongly correlated with SOC content whether corrected for clay content (SOC_adj R² = .571, p < .0001) or not (SOC_unadj R² = 0.490, p = .002). Time since tillage controlled SOC stocks and WSA scores, accounting for 75.5% and 51.3% of the total variation, respectively. We conclude that (1) SOC can be reliably measured in farmed soils using accepted protocols and related to land management and (2) WSA scores can be rapidly measured in clay soils and related to SOC stocks and soil management.     

土壤团聚体有机碳研究进展

土壤有机碳是衡量土壤肥力的重要指标,对于促进土壤养分循环、增加养分有效性有重要作用。土壤团聚体是土壤的重要组成部分,是组成土壤结构的最小单元,受到自然因素和人为因素的影响,其形成转化过程与土壤固碳过程息息相关,因而研究团聚体和有机碳的关系及团聚体有机碳影响因素对于土壤结构的改善和土壤质量的提升具有重要意义。本文通过对文献的总结,明晰了土壤团聚体和有机碳的关系,阐述了土壤类型、施肥方式、土地利用和矿区复垦对土壤团聚体有机碳的影响,并从生物质炭的长期定位研究和复垦矿区的土壤修复两方面对土壤团聚体有机碳的研究进行展望,研究结果可为合理的农业生产提供科学依据。     

外源褪黑素对干旱胁迫下大豆鼓粒期生理和产量的影响

干旱胁迫降低大豆产量,探究提高大豆耐旱能力和降低产量损失的机制对大豆生产具有重要意义。施褪黑素能缓解干旱胁迫对植株生长的抑制和氧化损伤。本试验于2017—2018年研究叶面喷施褪黑素对干旱胁迫下大豆鼓粒期叶片光合、抗逆、碳氮代谢和产量的影响表明,外源褪黑素提高干旱胁迫下大豆叶片抗氧化酶活性,抑制活性氧的产生和细胞膜损伤,缓解干旱胁迫对光合能力的抑制,提高碳氮同化能力,最终缓解干旱胁迫造成的产量损失。与干旱胁迫相比,褪黑素处理下单株荚数、单株粒数和百粒重两年平均提高了2.9%、0.8%和17.2%,产量(单株粒重)平均提高了14.7%。     

Do tillage and conversion of grassland to cropland always deplete soil organic carbon?

ABSTRACT

Conversion of grassland to cropland is widely reported to deplete soil organic carbon (SOC) largely due to tillage effects on the decomposition of SOC. However, most studies report on long-term changes in SOC following the conversion and little is known about the changes in the short term. Net ecosystem carbon budget (NECB) measures the difference between total C input (i.e., manure, above- and below-ground plant residues) and C loss through heterotrophic respiration (RH). However, most studies that report temporal SOC do not report other components of the NECB like RH, total C inputs and often do not include the cumulative annualized change of these components. This review evaluated the change in C input, RH, NECB and SOC after conversion of permanent/continuous grassland to cropland within 5 years after the conversion. We also reviewed and compared no-tillage and conventional tillage on SOC storage and accumulation. Total C input was higher in grassland than cropland largely due to high root biomass, as opposed to aboveground residue, and therefore grassland tended to have higher NECB. Despite higher NECB in grassland, the SOC stocks in cropland (cornfield) converted from grassland were greater than that in continuous grassland within first 2–3 years of conversion. The combination of manure C addition and tillage in cropland showed potential to maintain NECB and increase SOC. Within the continuous grassland C addition alone increased NECB but did not result in a corresponding increase in SOC. Residue retention and manure addition are recognized as good practices for increasing SOC, this study however, shows that combining them with occasional tillage, especially in managed grasslands, could increase the rate of SOC storage in soils.     

板式家具设计与制造中的减碳技术与应用

随着我国对环保的日益重视,以人造板为主要原料的板式家具适应绿色健康发展理念。介绍了板式家具主要材料以及板式家具主要原材料分类,分析了板式家具设计与制造中的减碳技术,为板式家具设计及制造企业能获得更好的社会和经济效益提供参考。     

一氧化碳(CO)在植物体内的生理生化作用研究进展

为了促进一氧化碳(CO)在植物生理生化方面的研究,本文归纳了CO在植物体中的生物合成途径,CO作为信号分子对植物各种生理功能的调控,以及CO与其他信号分子之间的相互作用。经过分析得出,CO在植物生物胁迫过程中的作用及其作用机制方面的研究还很少,因此,CO在这方面的研究将会成为今后的研究重点。     

无机碳源对零价铁介导的自养脱氮序批式反应器处理高氨氮废水的影响

无机碳源作为自养微生物的能量来源,是影响自养脱氮细菌富集的重要因素。文章通过添加不同量的KHCO3作为ZVI介导的自养脱氮体系中无机碳源,研究反应体系的脱氮效果影响趋势以及适宜的无机碳源添加量。结果如下:1)KHCO3作为无机碳源可以显著提高NH^+4-N去除率,KHCO3添加量越多,其NH^+4-N去除率越高。KHCO3添加量分别为2 g,1 g,0.5 g的SBR反应器R2,R1,R0.5的NH^+4-N去除率分别为98.39%,65.18%,44.56%,相较不添加KHCO3的R0分别提高86.5%,53.29%,32.67%。ZVI的添加会降低KHCO3对NH^+4-N氧化的促进作用。2)KHCO3可明显提高TIN去除效果,促进总氮脱除的高低顺序是R1>R0.5>R2,SBR反应器R2,R1,R0.5的平均TIN去除率分别为19.01%,32.04%,27.62%,相较于空白组R0分别提高了10.60%,23.63%,19.21%。3)KHCO3可中和硝化反应产生的H^+,对反应体系具有缓冲作用,可使微生物处于较适宜的酸碱环境中,更有利于反应器的稳定运行。4)适量的无机碳源KHCO3可以促进氨氧化细菌和厌氧氨氧化细菌的活性。该研究探讨了无机碳源在零价铁脱氮体系中的影响趋势,为铁型脱氮技术提供了理论支撑。     

海口市林分碳密度与景观格局指数耦合研究

为了解森林景观的空间组成、分布等特征对林分碳密度的影响，并以此为海口市优化林分结构，保护林地资源等方面提供参考。以海口市2015年森林资源二类调查数据为基础，运用arcgis、fragstats、spss等软件量化林分碳密度与景观格局指数并以此构建耦合协调度模型，来反映林分碳密度与森林景观格局的关系。研究发现，海口市热带林面积比重较大，且人为经营活动较强，导致其景观破碎化程度较高；林分碳密度与森林景观格局指数之间具有一定的相关性，且是相互促进的关系，当某一林分类型的空间配置较好，分布较聚集，不被其他地类分割时，其碳密度往往也较高。通过对海口市林分碳密度和森林景观格局指数的耦合研究，发现其林分碳密度与森林景观格局指数耦合协调度状况总体上并不良好，需要进行调整和改善。