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91.
Common bean (Phaseolus vulgaris L.) is the most important food legume, cultivated by small farmers and is usually exposed to unfavorable conditions with minimum use of inputs. Drought and low soil fertility, especially phosphorus and nitrogen (N) deficiencies, are major limitations to bean yield in smallholder systems. Beans can derive part of their required N from the atmosphere through symbiotic nitrogen fixation (SNF). Drought stress severely limits SNF ability of plants. The main objectives of this study were to: (i) test and validate the use of 15N natural abundance in grain to quantify phenotypic differences in SNF ability for its implementation in breeding programs of common bean with bush growth habit aiming to improve SNF, and (ii) quantify phenotypic differences in SNF under drought to identify superior genotypes that could serve as parents. Field studies were conducted at CIAT-Palmira, Colombia using a set of 36 bean genotypes belonging to the Middle American gene pool for evaluation in two seasons with two levels of water supply (irrigated and drought stress). We used 15N natural abundance method to compare SNF ability estimated from shoot tissue sampled at mid-pod filling growth stage vs. grain tissue sampled at harvest. Our results showed positive and significant correlation between nitrogen derived from the atmosphere (%Ndfa) estimated using shoot tissue at mid-pod filling and %Ndfa estimated using grain tissue at harvest. Both methods showed phenotypic variability in SNF ability under both drought and irrigated conditions and a significant reduction in SNF ability was observed under drought stress. We suggest that the method of estimating Ndfa using grain tissue (Ndfa-G) could be applied in bean breeding programs to improve SNF ability. Using this method of Ndfa-G, we identified four bean lines (RCB 593, SEA 15, NCB 226 and BFS 29) that combine greater SNF ability with greater grain yield under drought stress and these could serve as potential parents to further improve SNF ability of common bean. 相似文献
92.
首先分析了现阶段中国农业院校提高农业科技成果转化效率的现实意义,在此基础上以中国H农业大学为例,深入研究了中国农业院校在农业科技成果转化工作中存在的问题,并针对性地提出了解决对策。 相似文献
93.
太原经济技术开发区用地效益评价 总被引:1,自引:1,他引:0
通过对太原经济技术开发区的实际调查和对2002—2011年10 a间的相关统计及国家商务部历年发布的国家级经济技术开发区发展报告的信息进行分析,从开发区土地利用现状、年度建设用地供给、科工贸收入、工业总产值、GDP、税收收入、国内外资金利用等方面,综合评价了太原经济技术开发区的经济效益和用地效益。结果表明,该区独立运行10 a来成绩显著,整体效益逐步提高,在山西所有开发区中经济效益名列前茅,在全省经济技术开发区中每年的综合评价都名列第1;与国内中西部或中部的同类开发区相比,该区经济总量和单位面积产生的效益排名中后;与国内先进经济技术开发区相比,差距较大;该区内部分企业规模大、影响广泛,经济效益和用地效益均好,起到了带头和示范作用,但仍有部分企业规模小、投入水平低、建设周期长、产生效益低,影响了全区整体效益的发挥。建议开发区管委会引导入区企业加大投入,加快建设步伐,及早产生经济效益;尽快实施扩区计划,保证经济快速、健康发展;落实土地供给和退出政策,使有限的土地发挥更大的效益。 相似文献
94.
阐明长期有机物料施肥下土壤CO2排放特征及其影响机制以及碳库管理指数对黄土高原旱作农业区固碳减排及施肥模式选择的影响尤为重要。基于2012年设置在陇中黄土高原旱作区的长期定位试验,通过不施肥(CK)、氮肥(NF)、有机肥(OM)、秸秆(ST)、有机肥结合无机肥(OMNF)5个处理,测定并计算了2018年不同施肥措施下全年土壤CO2排放、作物碳排放效率和碳库管理指数的变化,并运用结构方程模型分析了0~30 cm土壤温度、水分、微生物量碳氮、易氧化有机碳、蔗糖酶、脲酶与土壤CO2排放速率的关系。结果表明:1)与不施肥相比,秸秆、有机结合无机肥和有机肥处理使生育期土壤CO2排放平均速率提高了42.72%、30.82%和29.79%,秸秆、有机肥处理分别使生育期土壤CO2排放量显著提高36.35%、32.45%(P<0.05),有机结合无机肥处理使碳排放效率显著降低41.10%(P<0.05);2)有机物料处理均能显著提高0~5 cm土层易氧化有机碳、微生物量碳氮、蔗糖酶活性和碳库管理指数,相比不施肥和氮肥处理,有机结合无机肥处理分别使0~30 cm土壤碳库管理指数提高127.41%,99.33%(P<0.05);3)结构方程模型表明,环境因子对土壤CO2排放速率的总解释度为53%,对土壤CO2排放速率总效应较大的影响因素包括土壤温度(2.36)、微生物量碳(1.59)和土壤水分(1.18),且均间接地影响着土壤CO2排放速率,土壤温度促进了微生物量碳和蔗糖酶活性的提高,微生物量碳促进了微生物量氮和易氧化有机碳的增加。综合来看,有机结合无机肥处理可以提升土壤碳库管理指数,保持微生物活性,增加作物产量,降低土壤碳排放效率,是陇中黄土高原旱作农业区比较适宜的农田培肥措施。 相似文献
95.
为了探究贵州喀斯特区域不同土壤利用方式对土壤质量的影响,我们对该地区的林地、人工草地、天然草地、农田、弃耕地5种土地利用方式下的土壤理化性质进行研究。基于最小数据集对该区域的土壤质量进行评价,构建的最小数据集包括:土壤pH值、容重、全盐、阳离子交换量、全氮、有效铜、有效铁等指标。结果表明:全量数据集和最小数据集获得的土壤质量均表现为林地 > 人工草地 > 天然草地 > 农田 > 弃耕地;人工草地、天然草地、农田、林地的土壤质量等级为二级,位于土壤质量分级中的"较高"水平,弃耕地土壤质量为三级,位于"中等"水平。以上结果表明,人为对自然生态系统的开垦降低了土壤的质量。 相似文献
96.
高产棉花太阳辐射能利用率及干物质分配规律研究 总被引:6,自引:0,他引:6
通过对1988~1989年高产棉花栽培试验结果进行分析发现,棉花的太阳辐射利用率在叶面积系数小于2.0时随叶面积系数的增加而线性增加,大于2.0时增加变缓。从生育时间看,7月中旬前太阳辐射利用率指数上升,7月中旬至8月底相对稳定在1.2~1.4克/兆焦左右,9月以后又不同程度线性下降。生长季内子棉太阳辐射经济效率1988和1989年分别为0.14和0.15克/兆焦。收获指数与最大叶面积系数呈显著负相关;盛花期之前棉株各器官之间的同伸关系或明显,盛花期后器官的生长相互间无明显的确定性关系。如能调节密度与叶面积系数的关系,使得既提高5~6月的辐射能利用率,同时使7~8月叶面积系数维持在3.0~3.5的适宜范围内,9~10月群体又不早衰,则有利于获得高产。 相似文献
97.
本文对太阳能的起源、传播、与物质的相互作用以及储存和利用等各个方面所涉及的物理学定律,特别是对太阳能热利用所涉及的热力学定律进行了概括和归纳。根据热力学定律指出太阳能热利用的真正适用范围。 相似文献
98.
Joo Carlos de Moraes S Lucien Sguy Florent Tivet Rattan Lal Serge Bouzinac Paulo Rogrio Borszowskei Clever Briedis Josiane Burkner dos Santos Daiani da Cruz Hartman Clayton Giani Bertoloni Jadir Rosa Theodor Friedrich 《Land Degradation \u0026amp; Development》2015,26(6):531-543
The continuous use of plowing for grain production has been the principal cause of soil degradation. This project was formulated on the hypothesis that the intensification of cropping systems by increasing biomass‐C input and its biodiversity under no‐till (NT) drives soil restoration of degraded agro‐ecosystem. The present study conducted at subtropical [Ponta Grossa (PG) site] and tropical regions [Lucas do Rio Verde, MT (LRV) site] in Brazil aimed to (i) assess the impact of the continuous plow‐based conventional tillage (CT) on soil organic carbon (SOC) stock vis‐à‐vis native vegetation (NV) as baseline; (ii) compare SOC balance among CT, NT cropping systems, and NV; and (iii) evaluate the redistribution of SOC stock in soil profile in relation to soil resilience. The continuous CT decreased the SOC stock by 0·58 and 0·67 Mg C ha−1 y−1 in the 0‐ to 20‐cm depth at the PG and LRV sites, respectively, and the rate of SOC sequestration was 0·59 for the PG site and ranged from 0·48 to 1·30 Mg C ha−1 y−1 for the LRV site. The fraction of C input by crop residues converted into SOC stock was ~14·2% at the PG site and ~20·5% at the LRV site. The SOC resilience index ranged from 0·29 to 0·79, and it increased with the increase in the C input among the NT systems and the SOC sequestration rates at the LRV site. These data support the hypothesis that NT cropping systems with high C input have a large potential to reverse the process of soil degradation and SOC decline. Copyright © 2013 John Wiley & Sons, Ltd. 相似文献
99.
Kleber Trabaquini Antnio Roberto Formaggio Lênio Soares Galvo 《Land Degradation \u0026amp; Development》2015,26(4):397-408
Soils from central Brazil have been intensively used over the last decades because of the rapid conversion of savannas ( Cerrado ) into corn/soybean fields. The objective of this work is to study modifications in the physical properties of soils in the Rio Verde watershed, as a function of the land use time for agriculture, determined from classification of Landsat satellite images between 1980 and 2010. Soil samples were collected at surface (0–20 cm) and subsurface (20–40 cm) horizons for the different classes of land use time (<10, 10–20, 20–30, and >30 years). The following physical properties were measured: bulk density (BD), air permeability (Ka), penetration resistance (PR), microporosity (MI), macroporosity (MA), and total porosity (TP). Results showed a strong expansion with time of agriculture that occupied 35·3% (1980), 37·4% (1990), 51·3% (2000), and 60·9% (2010) of the watershed area. When properties were compared with those from the reference areas (preserved soils under native vegetation), significant differences were observed for all the physical attributes of soils for a land use time higher than 20 years. Overall, BD and PR increased with land use time, and the opposite was verified for Ka, MA, and TP. Some physical properties presented values (e.g., 1·54 g cm−3 for BD and 0.06 cm3 cm−3 for MA) close to the critical ones reported to affect crop development, but they were not still impacting on local soybean yield. Copyright © 2013 John Wiley & Sons, Ltd. 相似文献
100.
M. Muoz‐Rojas A. Jordn L. M. Zavala D. De la Rosa S. K. Abd‐Elmabod M. Anaya‐Romero 《Land Degradation \u0026amp; Development》2015,26(2):168-179
During the last few decades, land use changes have largely affected the global warming process through emissions of CO2. However, C sequestration in terrestrial ecosystems could contribute to the decrease of atmospheric CO2 rates. Although Mediterranean areas show a high potential for C sequestration, only a few studies have been carried out in these systems. In this study, we propose a methodology to assess the impact of land use and land cover change dynamics on soil organic C stocks at different depths. Soil C sequestration rates are provided for different land cover changes and soil types in Andalusia (southern Spain). Our research is based on the analysis of detailed soil databases containing data from 1357 soil profiles, the Soil Map of Andalusia and the Land Use and Land Cover Map of Andalusia. Land use and land cover changes between 1956 and 2007 implied soil organic C losses in all soil groups, resulting in a total loss of 16·8 Tg (approximately 0·33 Tg y−1). Afforestation increased soil organic C mostly in the topsoil, and forest contributed to sequestration of 8·62 Mg ha−1 of soil organic C (25·4 per cent). Deforestation processes implied important C losses, particularly in Cambisols, Luvisols and Vertisols. The information generated in this study will be a useful basis for designing management strategies for stabilizing the increasing atmospheric CO2 concentrations by preservation of C stocks and C sequestration. Copyright © 2012 John Wiley & Sons, Ltd. 相似文献