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31.
S.‐E. Jacobsen 《Journal of Agronomy and Crop Science》2011,197(5):390-399
In Bolivia, one of the world’s most important centres of plant domestication, there is growing awareness of the value of native Andean crops, both for domestic consumption and for market sale – notably the virtually boom‐like consumer demand for quinoa around the world. The southern altiplano of Bolivia, south of Oruro, relies almost purely on the production of quinoa and breeding of llamas, which have also been selected as the two commodities of priority to the government to increase the income of the country. Presently, however, quinoa is facing increasing problems in production, owing to its increasing export market and price. The flat areas around the salt desert of the southern altiplano, previously characterized by natural vegetation fed by the llamas, are being increasingly sown with quinoa, hence transformed into deserts, because intensive cultivation methods make the soil loose its fertility. Possible solutions to these problems will require extensive efforts in the south, in addition to various strategies, which also include other parts of the Bolivian altiplano and a strengthened focus on other Andean crops. 相似文献
32.
指出了太阳能吸附式制冷是极具发展前途的绿色环保、节能的制冷技术,为当前制冷技术研究中的热点和焦点。综合介绍了太阳能固体吸附式制冷技术的原理、现状、存在的问题及其解决的措施,并对其应用前景作了分析和展望。 相似文献
33.
34.
Limited effects of land use on soil dissolved organic matter chemistry as assessed by excitation–emission fluorescence spectroscopy and molecular weight fractionation
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P. Roberts J. M. Gibbons P. W. Hill D. L. Jones M. Farrell 《Soil Use and Management》2016,32(4):662-665
Dissolved organic matter (DOM) in soil solution represents a complex mixture of organic molecules and plays a central role in carbon and nitrogen cycling in plant–microbial–soil systems. We tested whether excitation–emission matrix (EEM) fluorescence spectroscopy can be used to characterize DOM and support previous findings that the majority of DOM is of high molecular weight (MW). EEM fluorescence spectroscopy was used in conjunction with MW fractionation to characterize DOM in soil solution from a grassland soil land management gradient in North Wales, UK. Data analysis suggested that three distinct fluorescence components could be separated and identified from the EEM data. These components were identified as being of humic‐like or fulvic‐like origin. Contrary to expectations, the majority of the fluorescence signal occurred in the small MW (<1 kDa) fraction, although differences between soils from the differently managed grasslands were more apparent in larger MW fractions. We conclude that following further characterization of the chemical composition of the fluorophores, EEM has potential as a sensitive technique for characterizing the small MW phenolic fraction of DOM in soils. 相似文献
35.
本文旨在研究等磷、钾量条件下,化肥减氮及有机肥不同用量配施对水稻产量及土壤养分的影响,试验共设6个处理,分别为T1∶80%N+20%有机肥;T2∶80%N+40%有机肥;T3∶70%N+60%有机肥;T4∶70%N+80%有机肥;T5∶60%化肥+100%有机肥;CK:100%N+0,对水稻生育期株高、群体动态、产量、构产因子以及秋季土壤养分含量进行分析,结果表明:1化肥减氮20%时,不会对水稻造成明显减产,且当有机肥配施量为500kg·mu-2时,水稻籽粒产量最高,为775.19kg·mu-2,比CK增产17.20%;2有机肥的施用能提高水稻基本苗,对水稻穗长有显著提高效果,对空秕率影响较大,对枝梗数影响最小;3化肥减氮+有机肥配施可以提高土壤肥力,增加土壤有机质含量,提高土壤碱解氮、速效钾含量。 相似文献
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37.
通过对该黑龙江省集贤县农村生活垃圾处理情况的调查,深切感到解决农村生活垃圾问题的重要性,对此提出了对策建议 相似文献
38.
Evaluating biodegradability of soil organic matter by its thermal stability and chemical composition
The stability of soil organic matter (SOM) as it relates to resistance to microbial degradation has important implications for nutrient cycling, emission of greenhouse gases, and C sequestration. Hence, there is interest in developing new ways to quantify and characterise the labile and stable forms of SOM. Our objective in this study was to evaluate SOM under widely contrasting management regimes to determine whether the variation in chemical composition and resistance to pyrolysis observed for various constituent C fractions could be related to their resistance to decomposition. Samples from the same soil under permanent pasture, an arable cropping rotation, and chemical fallow were physically fractionated (sand: 2000-50 μm; silt: 50-5 μm, and clay: <5 μm). Biodegradability of the SOM in size fractions and whole soils was assessed in a laboratory mineralization study. Thermal stability was determined by analytical pyrolysis using a Rock-Eval pyrolyser, and chemical composition was characterized by X-ray absorption near-edge structure (XANES) spectroscopy at the C and N K-edges. Relative to the pasture soil, SOM in the arable and fallow soils declined by 30% and 40%, respectively. The mineralization bioassay showed that SOM in whole soil and soil fractions under fallow was less susceptible to biodegradation than that in other management practices. The SOM in the sand fraction was significantly more biodegradable than that in the silt or clay fractions. Analysis by XANES showed a proportional increase in carboxylates and a reduction in amides (protein) and aromatics in the fallow whole soil compared to the pasture and arable soils. Moreover, protein depletion was greatest in the sand fraction of the fallow soil. Sand fractions in fallow and arable soils were, however, relatively enriched in plant-derived phenols, aromatics, and carboxylates compared to the sand fraction of pasture soils. Analytical pyrolysis showed distinct differences in the thermal stability of SOM among the whole soil and their size fractions; it also showed that the loss of SOM generally involved preferential degradation of H-rich compounds. The temperature at which half of the C was pyrolyzed was strongly correlated with mineralizable C, providing good evidence for a link between the biological and thermal stability of SOM. 相似文献
39.
通过对色谱条件和样品前处理方法进行优化,建立固相萃取—亲水作用色谱法测定香菇(Lentinula edodes)中硫杂脯氨酸的检测方法。优化后的色谱条件为:Inertsil HILIC 亲水作用色谱柱(4.6×250 mm,5μm)对样品进行分离测定,流动相采用乙腈-0.1%磷酸水(85∶15,v/v)等度洗脱,流速0.8 mL/min,检测波长193 nm,柱温30℃。前处理方法为:香菇样品采用甲醇-水(70∶30,v/v)提取,MAX阴离子固相萃取小柱进行净化处理,甲醇-1.0%甲酸(90∶10,v/v)作为洗脱剂对目标物进行洗脱。检测结果表明,硫杂脯氨酸在2~100μg/mL范围内呈良好的线性关系,相关系数为0.9998,加标回收率为96.3%~101.7%,相对标准偏差在1.3%~4.8%之间,检出限为0.76μg/g,定量限为2.31μg/g。该方法回收率高、简单、快速、无需衍生化,适用于香菇子实体硫杂脯氨酸的定量检测分析。 相似文献
40.
The majority of dead organic material enters the soil carbon pool following initial incorporation into microbial biomass. The decomposition of microbial necromass carbon (C) is, therefore, an important process governing the balance between terrestrial and atmospheric C pools. We tested how abiotic stress (drought), biotic interactions (invertebrate grazing) and physical disturbance influence the biochemistry (C:N ratio and calcium oxalate production) of living fungal cells, and the subsequent stabilization of fungal-derived C after senescence. We traced the fate of 13C-labeled necromass from ‘stressed’ and ‘unstressed’ fungi into living soil microbes, dissolved organic carbon (DOC), total soil carbon and respired CO2. All stressors stimulated the production of calcium oxalate crystals and enhanced the C:N ratios of living fungal mycelia, leading to the formation of ‘recalcitrant’ necromass. Although we were unable to detect consistent effects of stress on the mineralization rates of fungal necromass, a greater proportion of the non-stressed (labile) fungal necromass C was stabilised in soil. Our finding is consistent with the emerging understanding that recalcitrant material is entirely decomposed within soil, but incorporated less efficiently into living microbial biomass and, ultimately, into stable SOC. 相似文献