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。     

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.     

光电技术在农业工程中的应用与展望

我国是农业生产大国，农业种植面积和多种农产品产量居世界前列，但是我国农业生产自动化程度相对较低，农业效益提升潜力大。光电技术在提升农业效益方面大有可为。概述了光电技术在农业工程中的应用现状，并展望了光电技术在农业工程中的发展趋势。      

岩溶流域典型农业区水体氢氧同位素的空间异质性及形成机制

分别于平水期和枯水期采集了花溪河流域典型农业区地表水和地下水样品。利用氢氧同位素示踪技术,结合土地利用类型对研究区不同水体的补给来源、季节变化及主要影响过程进行了分析,并对不同水体氢氧同位素值进行了空间插值分析,同时对其形成机制进行了分析,阐明了不同土地利用类型影响下的主要水文过程。结果表明:(1)研究区不同水体的主要补给来源为当地大气降水,月亮湖水库受蒸发作用影响明显,地表水和地下水的δD和δ~(18)O整体上呈现平水期高于枯水期的特征。(2)地下水的δD和δ~(18)O在枯水期与平水期均呈现明显的空间分异性特征,西部水田/水库集中区富集,东部旱地集中区贫化,土地利用对研究区环境水文过程影响明显。该研究结果有助于了解不同土地利用方式下地表水对地下水的影响,为流域管理提供科学依据。     

乡土阔叶树种在碳汇造林中的应用及优势分析

随着我国社会经济的发展,逐步暴露出了许多的生态环境问题。而为了维持生态的平衡,就要提高植树造林的力度,这其中碳汇造林就是植树造林工作的延伸。在碳汇造林中乡土阔叶树种发挥着重要作用,针对乡土阔叶树种在碳汇造林中的应用进行分析,对项目中出现的问题进行优化。     

资本禀赋、技术认知与农户耕地低碳利用意愿

耕地低碳利用对于减少农业温室气体排放,促进农业持续健康发展具有积极意义。建立资本禀赋、技术认知的理论分析模型和研究假说,利用湖北省347户农户的调研数据,在测度农户资本禀赋、耕地低碳利用技术认知的基础上,采用Logit模型、中介效应模型、调节效应检验方法,就资本禀赋、技术认知与农户耕地低碳利用意愿的关系进行实证研究。结果发现,资本禀赋不仅对农户耕地低碳利用意愿在1%水平上有显著的直接正向影响,还会通过技术认知这一中介变量在1%水平上产生显著的间接正向影响,环境素养在农户自我效能认知和耕地低碳利用意愿间发挥正向调节作用。据此,建议从经济资本、社会资本、文化资本3个角度提升农户的资本禀赋,通过多种渠道提升农户对耕地低碳利用的认知水平,提高农户环境素养。     

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.     

Substitution of chemical fertilizer by Chinese milk vetch improves the sustainability of yield and accumulation of soil organic carbon in a double-rice cropping system

The double-rice cropping system is a very important intensive cropping system for food security in China. There have been few studies of the sustainability of yield and accumulation of soil organic carbon(SOC) in the double-rice cropping system following a partial substitution of chemical fertilizer by Chinese milk vetch(Mv). We conducted a 10-year(2008–2017) field experiment in Nan County, South-Central China, to examine the double-rice productivity and SOC accumulation in a paddy soil in response to different fertilization levels and Mv application(22.5 Mg ha~(–1)). Fertilizer and Mv were applied both individually and in combination(sole chemical fertilizers, Mv plus 100, 80, 60, 40, and 0% of the recommended dose of chemical fertilizers, labeled as F100, MF100, MF80, MF60, MF40, and MF0, respectively). It was found that the grain yields of double-rice crop in treatments receiving Mv were reduced when the dose of chemical fertilizer was reduced, while the change in SOC stock displayed a double peak curve. The MF100 produced the highest double-rice yield and SOC stock, with the value higher by 13.5 and 26.8% than that in the F100. However, the grain yields increased in the MF80(by 8.4% compared to the F100), while the SOC stock only increased by 8.4%. Analogous to the change of grain yield, the sustainable yield index(SYI) of double rice were improved significantly in the MF100 and MF80 compared to the F100, while there was a slight increase in the MF60 and MF40. After a certain amount of Mv input(22.5 Mg ha~(–1)), the carbon sequestration rate was affected by the nutrient input due to the stimulation of microbial biomass. Compared with the MF0, the MF100 and MF40 resulted in a dramatically higher carbon sequestration rate(with the value higher by 71.6 and 70.1%),whereas the MF80 induced a lower carbon sequestration rate with the value lower by 70.1% compared to the MF0. Based on the above results we suggested that Mv could partially replace chemical fertilizers(e.g., 40–60%) to improve or maintain the productivity and sustainability of the double-rice cropping system in South-Central China.     

科尔沁草甸湿地土壤碳氮剖面分布及生长季动态特征

采用定位观测的试验方法,于2016年5-10月及2017年8月对科尔沁草甸湿地0~100 cm土层土壤有机碳、全氮剖面分布及生长季动态特征进行了实验分析,旨在为科尔沁草甸湿地保护提供科学指导并为干旱半干旱地区湿地土壤碳氮储量估算提供借鉴。结果表明:1)科尔沁草甸湿地土壤有机碳、全氮含量整体随土层深度下降,0~20 cm土层间下降显著,20 cm以下趋于相对稳定,范围分别为11.9~23.5 g·kg^-1和0.66~1.50 g·kg^-1。2)各土层土壤碳氮含量月间差异显著(全氮40~60 cm土层除外),变化幅度随土层深度先减小后增大;土壤碳氮密度(100 cm)生长季变化大于年际变化,有机碳密度全生长季呈上升趋势,范围为15.44~20.82 kg·m^-2,全氮密度生长初期明显下降,之后趋于相对稳定,范围为1.01~1.16 kg·m^-2。3)土壤有机碳含量与全氮含量呈极显著正相关;植被和水文是影响其分布、变化的关键因子。科尔沁草甸湿地生长季土壤有机碳、全氮密度变化较大,且表现为潜在的碳汇和氮源,但年际间碳汇潜力未充分发挥,本研究建议禁牧力度应加大并增加氮肥投入以提高科尔沁草甸湿地生态系统功能。