GIS在生态土地分类中的作用

This paper depicted the physiographic landscape features and natural vegetation situation of study area (the eastern Jilin Province), and expatiates the definition, basic characters and its development of Ecological Land Classification (ELC). Based on the combination of relief map, satellite photography for study area and vegetation inventory data of 480 sample sites, a 5-class and a 15-class ecological land type map was concluded according to 4 important factors including slope, aspect, vegetation and elevation. Ecological Classification System (ECS) is a method to identify, characterize, and map ecosystems. The Ecological Land Type (ELT) was examined and applied initially in eastern Jilin Province. Foundation item: This paper was supported by Chinese Academy of Sciences “100 people” project and the Open Research Station of Changbai Mountain Forest Ecosystem. Biography: XIAO Bao-ying (1974-), female, postgraduate in Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, P. R. China Responsible editor: Zhu Hong     

使用GIS区划白河林业局森林经营类型

使用GIS区划了白河林业局森林经营类型,并和原有的森林经营类型进行了比较。在数字化区划的森林经营类型中,二级系统被采纳。首先,白河林业局被区划为林地和非林地,其中,总面积的96%为林地,然后,林地区划为重点公益林,一般公益林和商品林。在重新区划的森林经营类型中,商品林达到总面积的45.0%,是最主要的森林经营类型:重点公益林和一般公益林分别为总面积的21.2%和29.9%。两个区划结果有很大的不同,在数字化区划的森林经营类型中,各类型斑块数量较多,面积较小,这些不同主要由使用数据,区划单位和区划方法的不同引起的。研究表明,GIS在区划森林经营类型时是一种有效的方法,二类数据和其它类型数据的结合是必要的。图2表4参22。     

科尔沁草原主要草地植物传播生物学简析

本研究论述了科尔沁草原主要草地植物的传播生物学特性.在141种植物中,44种以种子作为传播体,97种以果实作为传播体;传播体重量< 0.1 mg的植物12种,重量0.1～0.999 9 mg的植物61种,重量1～9.999 9 mg的植物55种,重量10～99.999 9 mg的植物12种,重量100～999.999 9 mg的植物1种;具有典型聚合传播体的植物4种;具有典型多态传播体的植物1种;传播体具附属物的植物66种(占总数的46%),其中19种带冠毛,10种带绢毛或丝毛,15种带芒或刚毛,6种带翅,6种带钩或刺,10种带其他附属物(花柱、花萼、结块和喙等).在124种植物中,11种植物(7种蒿属植物、2种车前、百里香1种和野亚麻1种)种子具有粘液,其种子或果实的干重＜1 mg.已发现23种植物具有明显的植冠种子库(植冠种子库种子达到总结种量的5%).8种植物植冠种子库种子超过结种量的30%,7种植物达到结种量的20%～30%,8种植物少于结种量的20%.具有植冠种子库的植物以菊科(尤其蒿属)、禾本科和藜科植物为多.具有较强或相对较强沙生适应性的植物多数具有植冠种子库.探讨了传播体类型和重量、利于(或阻滞)传播的传播体特征、传播体多态性与传播适应的多面性、延缓传播与植冠种子库等方面的问题.     

Nitrous oxide emissions from dairy farm effluent applied to a New Zealand pasture soil

A field experiment on permanent ryegrass–white clover pasture at AgResearch's Ruakura dairy farm near Hamilton, New Zealand quantified nitrous oxide (N₂O) emissions from different types of dairy effluent applied to soil at three seasons and evaluated the potential of dicyandiamide (DCD) (a nitrification inhibitor) to decrease gaseous N₂O emissions. Fresh or stored manure and farm dairy effluent (FDE; from dairy shed washings), with or without DCD (10 kg/ha), were applied at approximately 100 kg N/ha to plots on a well‐drained soil on volcanic parent material. A field chamber technique was used to measure N₂O emissions. Application of manure or FDE, both in fresh and stored forms, to pasture generally increased N₂O emissions. Overall N₂O emission factors (EF) varied between 0.01% and 1.87%, depending on application season and effluent type. EFs in spring and autumn were greater than those in summer (P < 0.05). Among the effluents, N₂O EFs were largest from fresh FDE (1.65%) during the spring measurement period, stored manure (1.87%) during the autumn and stored FDE (0.25%) during the summer. DCD was effective in decreasing N₂O EFs from fresh FDE, fresh manure, stored FDE and stored manure by 40–80%, 69–76%, 24–84% and 60–70%, respectively. DCD reduced N₂O emissions during the spring and autumn seasons more effectively than in the summer season.     

Shifts in microbial diversity through land use intensity as drivers of carbon mineralization in soil

Land use practices alter the biomass and structure of soil microbial communities. However, the impact of land management intensity on soil microbial diversity (i.e. richness and evenness) and consequences for functioning is still poorly understood. Here, we addressed this question by coupling molecular characterization of microbial diversity with measurements of carbon (C) mineralization in soils obtained from three locations across Europe, each representing a gradient of land management intensity under different soil and environmental conditions. Bacterial and fungal diversity were characterized by high throughput sequencing of ribosomal genes. Carbon cycling activities (i.e., mineralization of autochthonous soil organic matter, mineralization of allochthonous plant residues) were measured by quantifying ¹²C- and ¹³C-CO₂ release after soils had been amended, or not, with ¹³C-labelled wheat residues. Variation partitioning analysis was used to rank biological and physicochemical soil parameters according to their relative contribution to these activities. Across all three locations, microbial diversity was greatest at intermediate levels of land use intensity, indicating that optimal management of soil microbial diversity might not be achieved under the least intensive agriculture. Microbial richness was the best predictor of the C-cycling activities, with bacterial and fungal richness explaining 32.2 and 17% of the intensity of autochthonous soil organic matter mineralization; and fungal richness explaining 77% of the intensity of wheat residues mineralization. Altogether, our results provide evidence that there is scope for improvement in soil management to enhance microbial biodiversity and optimize C transformations mediated by microbial communities in soil.     

稳定性肥料发展与展望

稳定性肥料的核心是脲酶抑制剂和硝化抑制剂，是指在肥料的生产过程中添加脲酶抑制剂或硝化抑制剂，或者同时添加两种抑制剂的肥料。其良好的农学效应和环境效益为实现农业节本增效提供重要途径。近年来稳定性肥料在基础科研和生产应用领域均发展较快，本文对国内外相关研究进行系统总结，并指出未来的发展方向。首先，回顾了抑制剂的研发、作用机理等方面的进展；其次，概述了稳定性肥料的品种、生产工艺、产能及推广应用情况；最后，对稳定性肥料应用后的作物产量和环境效应进行了阐述。为了促进稳定性肥料产业的健康持续发展，未来需要进一步加强环境友好型抑制剂品种的研发；重视抑制剂保护技术的研究，以解决抑制剂作用效果持久性和稳定性的问题；加强不同抑制剂配伍协同，抑制剂与增效剂复合作用机理与技术的研究；研究开发针对不同区域、不同作物的稳定性专用肥料。     

Soil aggregation: Influence on microbial biomass and implications for biological processes

Our 1988 paper, describing the effects of cultivation on microbial biomass and activity in different aggregate size classes, brought together the ‘aggregate hierarchy theory’ and the ‘microbial biomass concept’. This enabled us to identify the relationships between microbial and microhabitat (aggregate) properties and organic matter distribution and explain some of their responses to disturbance. By combining biochemical and direct microscopy based quantification of microbial abundance with enzyme activities and process measurements, this study provided evidence for the role of microbial biomass (especially fungi) in macroaggregate dynamics and carbon and nutrient flush following cultivation. In the last ten years environmental genomic techniques have provided much new knowledge on bacterial composition in aggregate size fractions yet detailed information about other microbial groups (e.g. fungi, archaea and protozoa) is lacking.We now know that soil aggregates are dynamic entities – constantly changing with regard to their biological, chemical and physical properties and, in particular, their influences on plant nutrition and health. As a consequence, elucidation of the many mechanisms regulating soil C and nutrient dynamics demands a better understanding of the role of specific members of microbial communities and their metabolic capabilities as well as their location within the soil matrix (e.g. aggregates, pore spaces) and their reciprocal relationship with plant roots. In addition, the impacts of environment and soil type needs to be quantified at the microscale using, wherever possible, non-destructive ‘in situ’ techniques to predict and quantify the impacts of anthropogenic activities on soil microbial diversity and ecosystem level functions.     

用于黑土的稳定性氯化铵的适宜硝化抑制剂和氮肥增效剂组合

【目的】本文研究添加不同种类硝化抑制剂的高效稳定性氯化铵氮肥在黑土中的施用效果，旨在筛选出适合旱作黑土的高效稳定性氯化铵态氮肥。【方法】在氯化铵中分别添加硝化抑制剂3,4-二甲基吡唑磷酸盐 (DMPP)、双氰胺 (DCD)、2-氯-6-三甲基吡啶 (Nitrapyrin，CP)、氨保护剂 (N-GD) 和1种氮肥增效剂 (HFJ) 及其组合，制成9种稳定性氯化铵氮肥。以不施氮肥 (CK) 和施普通氯化铵 (CK-N) 为对照，以9种稳定性氯化铵为处理进行了等氮量盆栽试验。在玉米苗期、大喇叭口期、灌浆期和成熟期测定了土壤中铵态氮和硝态氮含量，在玉米成熟期测定植株生物量、籽粒产量和氮素含量，计算铵态氮肥的表观硝化率、硝化抑制率、氮肥农学效率、氮肥偏生产力。【结果】1) 与CK-N处理相比，9个处理均显著提高玉米的产量，HFJ的效果均为最显著，可增加玉米籽粒产量3.99倍，提高氮肥吸收利用率4.98倍，显著高于8个硝化抑制剂处理 (P < 0.05)。CP + DMPP和CP + DCD处理提高玉米籽粒产量1.90～2.11倍，两个处理之间无显著差异；CP + DMPP玉米生物量显著高于CP处理，而与DMPP和DCD处理无显著差异；CP + DMPP玉米氮肥吸收利用率显著高于CP和DMPP处理，显著提高3.71倍 (P < 0.05)；2) CP + DMPP和CP + DCD土壤中铵态氮含量提高2.09～2.42倍，且显著高于CP、DMPP和DCD处理 (P < 0.05)，而硝态氮含量和土壤表观硝化率均显著降低24%和66%～68%，与CP和DCD处理存在显著差异 (P < 0.05)；苗期CP + DMPP和CP + DCD硝化抑制率高达23.9%～24.3%，显著高于CP和DCD (P < 0.05)。【结论】在黑土中，氯化铵中添加硝化抑制剂组合的硝化抑制率显著高于添加单一抑制剂，能够有效减缓土壤中铵态氮向硝态氮的转化，减少土壤中氮素损失，降低环境污染。CP + DMPP组合玉米的氮肥吸收利用率显著高于CP + DCD组合。氮肥增效剂HFJ显著增加玉米的氮素吸收量，提高氮肥利用率，从而使玉米获得高产并获得较高的收获指数和经济系数。因此，综合考虑产量和抑制硝化作用等因素，黑土区氯化铵作为玉米生产用氮肥时，建议首选添加氮肥增效剂HFJ来保证作物的高产和氮肥高利用率，也可以添加硝化抑制剂组合CP + DMPP，或者CP + DCD制备稳定性氯化铵来提高氯化铵的增产效果和氮肥利用率，减少氮素损失，降低环境污染。     

Greater humification of belowground than aboveground biomass carbon into particulate soil organic matter in no-till corn and soybean crops

Quantifying the amount of carbon (C) incorporated from decomposing residues into soil organic carbon (C_S) requires knowing the rate of C stabilization (humification rate) into different soil organic matter pools. However, the differential humification rates of C derived from belowground and aboveground biomass into C_S pools has been poorly quantified. We estimated the contribution of aboveground and belowground biomass to the formation of C_S in four agricultural treatments by measuring changes in δ¹³C natural abundance in particulate organic matter (C_POM) associated with manipulations of C₃ and C₄ biomass. The treatments were (1) continuous corn cropping (C₄ plant), (2) continuous soybean cropping (C₃), and two stubble exchange treatments (3 and 4) where the aboveground biomass left after the grain harvest was exchanged between corn and soybean plots, allowing the separation of aboveground and belowground C inputs to C_S based on the different δ¹³C signatures. After two growing seasons, C_POM was primarily derived from belowground C inputs, even though they represented only ∼10% of the total plant C inputs as residues. Belowground biomass contributed from 60% to almost 80% of the total new C present in the C_POM in the top 10 cm of soil. The humification rate of belowground C inputs into C_POM was 24% and 10%, while that of aboveground C inputs was only 0.5% and 1.0% for soybean and corn, respectively. Our results indicate that roots can play a disproportionately important role in the C_POM budget in soils. Keywords Particulate organic matter; root carbon inputs; carbon isotopes; humification rate; corn; soybean.