内蒙古高原紫花苜蓿土壤氮素丰缺指标和推荐施氮量

为了给内蒙古高原紫花苜蓿（Medicago sativa L.）测土施氮奠定科学基础，本研究采用“零散实验数据整合法”和“养分平衡-地力差减法”新应用公式，开展了该自然区域紫花苜蓿土壤氮素丰缺指标和推荐施氮量研究。结果表明：内蒙古高原生长第1年紫花苜蓿土壤碱解氮第1~6级丰缺指标为≥48，20~48，8~20，4~8，2~4和<2 mg·kg^-1，土壤全氮第1~5级丰缺指标为≥1.4，0.8~1.4，0.4~0.8，0.2~0.4和<0.2 g·kg^-1，土壤有机质第1~6级丰缺指标为≥17，10~17，6~10，3~6，2~3和<2 g·kg^-1。当紫花苜蓿目标产量9~18 t·hm^-2、氮肥利用率40%时，内蒙古高原紫花苜蓿第1~6级土壤推荐施氮量分别为0，68~135，135~270，203~405，270~540和338~675 kg·hm^-2。     

沉淀法制备的紫杉醇白蛋白微粒包封率测定

采用沉淀法制备紫杉醇白蛋白微粒,采用高效液相色谱法(HPLC)测定紫杉醇质量浓度,以二氯甲烷为有机相,采用萃取法分离白蛋白微粒与游离药物,测定其包封率。结果表明:紫杉醇在10~100 mg·L-1范围内线性良好,平均回收率可达到97.6%~101.0%;有机溶剂萃取法测定紫杉醇白蛋白微粒包封率的平均回收率,达94.80%~101.67%。这种方法测定紫杉醇白蛋白微粒回收率准确可靠,适用于沉淀法制备的白蛋白微粒的包封率测定。     

AMF促进植物吸收矿质元素的生理机制及对土壤硫素的影响

由于人口不断增长,人们要快速得到高产高质粮食的要求迫切,大量使用化肥,导致了有害物质残留,土壤或水污染,土壤板结或某些营养元素相对匮乏等一系列环境问题。丛枝菌根(Arbuscular mycorrhiza, AM)是土壤内常见的共生结构,由AM真菌(AMF)与土壤根系形成。已有研究表明其可通过分泌代谢物,增大根系与土壤接触面积,调节某些土壤元素存在形式等多种途径,影响植物对土壤元素的吸收转运。硫是维持植物生长发育的必需元素之一,可由于植物对S的需要并不如N,P,K大量,现代农业在对土壤进行施肥过程中往往将其忽略,因此土壤缺S正逐渐成为中国农业发展的限制因素。为了解决以上问题,本文将主要对AMF影响植物吸收土壤元素的途径及生理机制进行总结分析。并根据其作用方式特点进一步分析AM共生对植物吸收转运硫素的影响,指出AMF作为生物化肥的可行性,以期为解决现代化肥的替代问题以及土壤缺硫问题提供新的思路。     

不同有机物对铁皮石斛试管苗生长发育的影响

研究不同有机物浸提液对铁皮石斛试管苗生长的影响。在相同的培养条件下，以8种含有不同有机物的培养基培养试管苗，60d后对试管苗的各种性状进行记录统计，并与对照（没加有机物提取液）进行比较分析。结果不同的有机物浸提液对试管苗的影响效果不一样。壮苗以加入白萝卜提取液、CH和CM为佳，生根以加入香蕉提取液为佳，要提高繁殖系数以不加有机物为佳。     

碧峰峡森林土壤性状研究

碧峰峡不仅是旅游景点,还是多学科研究的天然“实验室”,地处雅安亚热带区,原始森林植被保护完好,土壤垂直分布明显,地质现象复杂,也是大熊猫、金丝猴出没之地。经研究结果：土壤呈酸性,自然肥力高．经相关分析结果：土壤有机质含量和ＣＥＣ等有关理化特性的相关性,较物理性粘粒与ＣＥＣ间更加显著。     

磷硫配施对冬小麦硒吸收及转运的影响

为了探讨磷硫配施对冬小麦产量、硒的吸收及转运的影响，为生产富硒小麦或合理调控小麦硒含量提供理论依据，采用盆栽试验，设置不同磷、硫水平，在小麦成熟期测定产量及植株各部位硒含量。结果表明：硫磷的配合施用能显著提高冬小麦产量，S0.1P0.4处理下冬小麦产量最高。除颖壳外，冬小麦各部位硒含量最高值都出现在S0P0处理。不论施硫与否，施磷均能显著降低冬小麦各部位硒含量，提高小麦植株硒累积量，促进冬小麦茎叶向颖壳的硒迁移，降低根向茎叶、颖壳向籽粒的硒迁移系数，还会减小籽粒的硒分配。单独施硫会降低植株的硒累积量，促进冬小麦根向茎叶、茎叶向颖壳的硒迁移，降低颖壳向籽粒的硒迁移系数，低硫处理能增加小麦籽粒的硒分配，高硫处理则降低了籽粒的硒分配。S0P0.2处理能显著提高籽粒硒累积量，而高浓度的磷硫配施会降低籽粒硒累积量；S0.1P0和S0.1P0.2处理籽粒硒分配较大,分别是45.3%和44.8%。因此，硫磷的合理配施能显著提高小麦产量，低硫（S0.1）高磷（P0.4）处理增产最显著。低硫（S0.1）低磷（P0.2）处理能更有效地增加植株硒累积量，增强硒在籽粒中的累积。     

Sewage sludge processing determines its impact on soil microbial community structure and function

Composting and thermal drying are amongst the most commonly used post-digestion processes for allowing sanitation and biological stabilization of sewage sludge from municipal treatment plants, and making it suitable as soil conditioner for use in agriculture. To assess the impact of sludge-derived materials on soil microbial properties, fresh (LAF), composted (LAC) and thermally dried (LAT) sludge fractions, each resulting from a different post-treatment process of a same aerobically digested sewage sludge, were added at 1% (w/w) application rate on two contrasting (a loam and a loamy sand) soils and incubated under laboratory conditions for 28 days. Soil respiration, microbial ATP content, hydrolytic activities and arginine ammonification rate were monitored throughout the incubation period. Results showed that soil biochemical variables, including the metabolic quotient (qCO₂), were markedly stimulated after sludge application, and the magnitude of this stimulatory effect was dependent on sludge type (precisely LAT > LAF > LAC), but not on soil type. This effect was related to the content of stable organic matter, which was lower in LAT. Genetic fingerprinting by PCR–DGGE revealed that compositional shifts of soil bacterial and, at greater extent, actinobacterial communities were responsive to the amendment with a differing sludge fraction. The observed time-dependent changes in the DGGE profiles of amended soils reflected the microbial turnover dependent on the sludge nutrient input, whereas no indications of adverse effects of sludge-borne contaminants were noted. Our findings indicate that composting rather thermal drying can represent a more appropriate post-digestion process to make sewage sludge suitable for use as soil conditioner in agriculture.     

Organic farming fosters agroecosystem functioning in Argentinian temperate soils: Evidence from litter decomposition and soil fauna

Benefits of organic farming on soil fauna have been widely observed and this has led to consider organic farming as a potential approach to reduce the environmental impact of conventional agriculture. However, there is still little evidence from field conditions about direct benefits of organic agriculture on soil ecosystem functioning. Hence, the aims of this study were to compare the effect of organic farming versus conventional farming on litter decomposition and to study how this process is affected by soil meso- and macrofauna abundances. Systems studied were: (1) organic farming with conventional tillage (ORG), (2) conventional farming with conventional tillage (CT), (3) conventional farming under no-tillage (NT), and (4) natural grassland as control system (GR). Decomposition was determined under field conditions by measuring weight loss in litterbags. Soil meso- and macrofauna contribution on decomposition was evaluated both by different mesh sizes and by assessing their abundances in the soil. Litter decomposition was always significantly higher after 9 and 12 months in ORG than in CT and NT (from 2 to 5 times in average), regardless decomposer community composition and litter type. Besides, mesofauna, macrofauna and earthworm abundances were significantly higher in ORG than in NT and CT (from 1.6 to 3.8, 1.7 to 2.3 and 16 to 25 times in average, respectively for each group). These results are especially relevant firstly because the positive effect of ORG in a key soil process has been proved under field conditions, being the first direct evidence that organic farming enhances the decomposition process. And secondly because the extensive organic system analyzed here did not include several practices which have been recognized as particularly positive for soil biota (e.g. manure use, low tillage intensity and high crop diversity). So, this research suggests that even when those practices are not applied, the non-use of agrochemicals is enough to produce positive changes in soil fauna and so in decomposition dynamics. Therefore, the adoption of organic system in an extensive way can also be suggested to farmers in order to improve ecosystem functioning and consequently to achieve better soil conditions for crop production.