脲酶抑制剂氢醌对土壤脲酶活性,氨挥发和硝化的抑制动态

1.氢醌对土壤脲酶活性的抑制率及其持续的时间同氢醌浓度成正相关,与土壤脲酶活性成负相关。2.氢醌能有效地抑制施入土壤中尿素氨的挥发,而对铵盐和尿素的硝化强度产生强烈抑制。3.在麦秸还田土壤中,由于脲酶活性增高而提高了施入尿素的水解速度,故需提高氢醌用量;但由于麦秸的“氮因子效应”又固定了尿素分解产物及其氧化产物,从而弥补了氢醌失效后可能造成氮素的继续损失。     

与氮转化有关的土壤酶活性对抑制剂施用的响应

利用室内模拟培养试验,研究好气条件下施用尿素后土壤脲酶、脲酸还原酶、亚硝酸还原酶和羟胺还原酶活性对脲酶抑制剂氢醌（HQ）与硝化抑制剂包被碳化钙（ECC）和双氰胺（DCD）组合（HQ ECC、HQ DCD）的响应、结果表明,HQ DCD组合与其它抑制剂处理相比能更有效地降低土壤脲酶活性,增加硝酸还原酶、亚硝酸还原酶、羟胺还原酶活性,不同处理土壤脲酶、亚硝酸还原酶和羟胺还原酶活性与土壤NH4^ 、NO3^-、NH3挥发和N2O排放速率间存在不同形式的显著相关关系：土壤脲酶、亚硝酸还原酶和羟胺还原酶活性之间存在不同形式的显著正相关关系。     

高寒灌丛生长季土壤转化酶与脲酶活性对增温和植物去除的响应

对青藏高原东缘窄叶鲜卑花土壤转化酶与脲酶活性对增温(0.6～1.3 ℃)和植物去除的响应进行研究,以了解气候变暖和植被干扰对高寒灌丛生长季不同时期土壤生态过程的影响.结果表明: 增温在整个生长季节使去除/不去除植物处理土壤转化酶活性显著增加了3.7%～13.3%.增温除在生长季末期对不去除植物处理土壤脲酶活性影响不显著以外,在其他时期使去除/不去除植物处理土壤脲酶活性显著增加10.8%～56.3%.去除植物处理对土壤转化酶与脲酶活性的影响因增温与生长季节而存在显著差异.去除植物显著降低了不增温样方生长季初期和末期与增温样方整个生长季节土壤转化酶活性,而没有显著影响生长季中期不增温样方土壤转化酶活性.去除植物仅在生长季末期使不增温样方土壤脲酶活性显著降低了10.5%;而在增温样方,去除植物仅在生长季初期和中期使土壤脲酶活性显著降低16.0%～18.7%.以上结果有利于全面认识高寒灌丛生态系统土壤碳氮循环过程.     

柑桔园土壤脲酶活性年周期变化及脲酶抑制剂氢醌的效应

本研究初步探明南亚热带赤红壤柑桔园土壤脲酶活性的年周期变化:冬季最低,春季升至高峰,夏季开始下降,直至秋季仍处于较低水平。室内模拟试验表明:氢醌对柑桔园土壤脲酶活性有明显抑制作用,其抑制率随浓度提高而增加,且随着培养时间的延长而逐渐下降;添加氢醌处理的尿素水解持续时间,比不加氢醌的延长约1倍。     

脲酶抑制剂和硝化抑制剂的协同作用对尿素氮转化和N2O排放的影响

根据培养试验,论述了脲酶抑制剂氢醌和硝化抑制剂双氰胺和碳化钙的不同组合在土壤正常水分和渍水的条件下对于土中尿素的水解及其释出的氨的吸附、氧化和挥发以及Ｎ２Ｏ生成的影响．文章指出,配合使用氢醌和双氰胺既能延缓土中尿素的水解并使水解后释出的氨在土中得以更多和更长时间的保持,还能减少土中硝酸盐的累积、氨挥发的损失及Ｎ２Ｏ的生成．这表明在脲酶抑制剂和硝化抑制剂间可能存在一定的协同作用．很好利用这一作用,将有益于提高尿素肥效和减少其Ｎ损失与环境污染．     

间甲酚及施磷对小麦间作蚕豆土壤微生物和酶活性的影响

通过盆栽试验,研究了不同磷水平下化感物质间甲酚对小麦间作蚕豆和单作小麦、单作蚕豆土壤微生物和酶活性的影响。结果表明,间甲酚对不同模式生长盛期细菌和微生物总数表现为化感促进作用,对真菌表现为化感抑制作用,随施磷量的增加间甲酚对土壤微生物的化感促进作用降低;不同模式生长盛期土壤微生物数量在施磷量为100mg／kg土的处理中最高,但成熟期施磷量为200mg／kg土的处理最高;间作较单作具有保持较高土壤细菌和微生物总数的作用,施磷水平越高间作增大微生物数量的效果越大;间甲酚对土壤微生物多样性具有明显降低作用,间作土壤的微生物多样性低于单作。间作具有较高的弱化间甲酚对土壤过氧化氢酶化感负效应的作用,施磷可增强土壤过氧化氢酶活性;磷素作用下土壤脲酶活性增强,间甲酚对单作蚕豆和间作土壤脲酶活性具有促进作用,但弱化了施磷对脲酶活性的增强作用;增施磷肥可弱化间甲酚对单作蚕豆和间作土壤酸性磷酸酶的化感负效应,对单作小麦土壤酸性磷酸酶活性的影响相反。间甲酚对不同模式土壤微生物和酶活性的影响在作物成熟期显著下降,说明随时间的推移土壤中间甲酚的作用力在不断弱化。     

碳添加下黑钙土胞内、胞外脲酶活性变化及其机制

土壤脲酶作为能够催化尿素水解的最重要酶类,对草地生态系统氮素供应具有重要作用。目前探讨不同碳添加对草地土壤胞外脲酶影响的研究报道相对较多,但碳添加对土壤胞内脲酶的影响,以及胞内和胞外脲酶对碳添加的响应是否一致等尚需深入研究。本研究依托额尔古纳森林草原过渡带生态系统研究站开展的碳添加野外试验平台(以葡萄糖为碳源),选取无碳添加(C₀)、250(C₂₅₀)和500(C₅₀₀) kg C·hm^-2·a^-1处理为供试对象,探讨碳添加下黑钙土胞内、胞外脲酶活性响应及其与土壤性质的关系。结果表明: 碳添加显著提高了土壤胞内脲酶活性,增加了土壤胞内脲酶活性占总脲酶活性的比例,但对土壤胞外脲酶活性没有显著影响。土壤胞内脲酶活性与微生物生物量具有显著正相关关系,表明胞内脲酶活性增加主要是由微生物生物量增加引起的。结构方程模型(SEM)分析表明,碳添加通过影响土壤微生物生物量间接提高了土壤胞内脲酶活性。     

脲酶抑制剂氢醌对土壤尿素氮转化的影响

本文根据用标记和非标记尿素进行的培养试验,论述了氢醌对于尿素的水解、氨的释出和挥发、硝化和反硝化作用以及生物固持的影响。得出的结论是:氢醌的作用不仅在于延缓尿素的水解和减少随之而来的氨的挥发,更重要的,是影响了尿素水解产物进一步转化的进程,增强了尿素氮对于作物的有效持续供应和减少了它的总损失。本文认为,在脲酶抑制剂的研究中,着眼点当不仅在于它们的直接作用,而更需要涉及对尿素氮转化的一系列过程的影响。这样,才能对抑制剂的作用机理有更深入的了解,对它的作用效果有更全面的评价。     

施用缓/控释尿素对玉米苗期土壤生物学活性的影响

采用盆栽试验,模拟田间生态环境,研究了施用不同种缓/控释氮素底肥对玉米苗期土壤硝酸还原酶、脲酶活性及微生物量碳、氮的影响.结果表明,施用硝化抑制剂(双氰胺)和脲酶抑制剂(n-丁基硫代磷酰三胺)涂层大颗粒尿素肥料的土壤硝酸还原酶活性最高;施用大颗粒尿素,脲酶活性最强,微生物量碳、氮最高.施用醋酸酯淀粉包膜大颗粒尿素、包膜双氰胺涂层大颗粒尿素、丙烯酸树脂包膜双氰胺涂层大颗粒尿素与不施氮肥土壤脲酶活性较高;每种处理微生物量碳与氮变化完全一致.施用醋酸酯淀粉包膜硝化和脲酶抑制剂涂层大颗粒尿素肥料,土壤微生物量碳、氮最低.同种膜材料包膜抑制剂涂层大颗粒尿素制成的缓/控释氮肥,对土壤生物学活性的影响效果好于直接包膜大颗粒尿素;丙烯酸树脂包膜大颗粒尿素制成的缓/控释氮肥,对氮素的控释效果明显好于醋酸酯淀粉包膜.     

沈北新区不同利用类型土壤脲酶活性及其影响因素分析

采用均匀网格布点法采集沈阳市沈北新区不同土地利用类型101个表层(0—20 cm)土壤样品, 测定了土壤脲酶活性、土壤理化性质和土壤细菌群落组成, 分析了不同利用类型土壤脲酶活性变化特征及其与土壤理化性质、土壤细菌优势菌群之间的关系。土壤酶活力测定结果表明, 沈北新区不同利用类型土壤脲酶活性由高到低依次为: 旱田>天然林地>城市绿地>水田; 相关分析与通径分析结果表明, 土壤脲酶活性与土壤含水量呈极显著负相关关系, 与总磷呈显著正相关关系, 含水量和总磷对土壤脲酶活性的影响除了直接效应外, 还存在较强的通过其它因素的间接效应, 说明它们是影响土壤脲酶活性的两个主要因素; 冗余分析结果表明, 放线菌门(Actinomycetes)、泉古菌门(Crenarchaeota)和酸杆菌门(Acidobacteria)对土壤脲酶影响较大, 其菌群丰度主要受土壤含水量的调控, 且其随土壤含水量的变化特征与土壤脲酶活性变化趋势相一致, 提示这些菌群可能是土壤脲酶的重要来源。     

Impact of rhizobial inoculation on Acacia senegal (L.) Willd. growth in greenhouse and soil functioning in relation to seed provenance and soil origin

Rhizobial inoculation has a positive impact on plants growth; however, there is little information about its effect on soil microbial communities and their activity in the rhizosphere. It was therefore necessary to test the effect of inoculation of Acacia senegal (L.) Willd. seedlings with selected rhizobia on plant growth, structure and diversity of soil bacterial communities and soil functioning in relation to plant provenance and soil origin. In order to carry out this experiment, three A. senegal seeds provenance from Kenya, Niger, and Senegal were inoculated with selected rhizobial strains. They have been further grown during 4 months in greenhouse conditions in two non-disinfected soils, Dahra and Goudiry coming respectively from arid and semi-arid areas. The principal component analysis (ACP) showed an inoculation effect on plant growth, rhizospheric bacterial diversity and soil functioning. However, the performances of the rhizobial strains varied in relation to the seed provenance and the soil origin. The selected rhizobial strains, the A. senegal provenance and the soil origin have modified the structure and the diversity of soil bacterial communities as measured by principal component analysis/denaturing gradient gel electrophoresis analyses. It is interesting to note that bacterial communities of Dahra soil were highly structured according to A. senegal provenance, whereas they were structured in relation to rhizobial inoculation in Goudiry soil. Besides, the impact of inoculation on soil microbial activities measured by fluorescein diacetate analyses varied in relation to plant provenance and soil origin. Nevertheless, total microbial activity was about two times higher in Goudiry, arid soil than in Dahra, semi-arid soil. Our results suggest that the rhizobial inoculation is a suitable tool for improving plants growth and soil fertility. Yet, the impact is dependent on inoculants, plant provenance and soil origin. It will, therefore, be crucial to identify the appropriate rhizobial strains and plant provenance or species in relation to the soil type.     

Effects of Added Organic Matter and Water on Soil Carbon Sequestration in an Arid Region

It is generally predicted that global warming will stimulate primary production and lead to more carbon (C) inputs to soil. However, many studies have found that soil C does not necessarily increase with increased plant litter input. Precipitation has increased in arid central Asia, and is predicted to increase more, so we tested the effects of adding fresh organic matter (FOM) and water on soil C sequestration in an arid region in northwest China. The results suggested that added FOM quickly decomposed and had minor effects on the soil organic carbon (SOC) pool to a depth of 30 cm. Both FOM and water addition had significant effects on the soil microbial biomass. The soil microbial biomass increased with added FOM, reached a maximum, and then declined as the FOM decomposed. The FOM had a more significant stimulating effect on microbial biomass with water addition. Under the soil moisture ranges used in this experiment (21.0%–29.7%), FOM input was more important than water addition in the soil C mineralization process. We concluded that short-term FOM input into the belowground soil and water addition do not affect the SOC pool in shrubland in an arid region.     

Soil microbial properties and plant growth responses to carbon and water addition in a temperate steppe: the importance of nutrient availability

Background

Global climatic change is generally expected to stimulate net primary production, and consequently increase soil carbon (C) input. The enhanced C input together with potentially increased precipitation may affect soil microbial processes and plant growth.

Methodology/Principal Findings

To examine the effects of C and water additions on soil microbial properties and plant growth, we conducted an experiment lasting two years in a temperate steppe of northeastern China. We found that soil C and water additions significantly affected microbial properties and stimulated plant growth. Carbon addition significantly increased soil microbial biomass and activity but had a limited effect on microbial community structure. Water addition significantly increased soil microbial activity in the first year but the response to water decreased in the second year. The water-induced changes of microbial activity could be ascribed to decreased soil nitrogen (N) availability and to the shift in soil microbial community structure. However, no water effect on soil microbial activity was visible under C addition during the two years, likely because C addition alleviated nutrient limitation of soil microbes. In addition, C and water additions interacted to affect plant functional group composition. Water addition significantly increased the ratio of grass to forb biomass in C addition plots but showed only minor effects under ambient C levels. Our results suggest that soil microbial activity and plant growth are limited by nutrient (C and N) and water availability, and highlight the importance of nutrient availability in modulating the responses of soil microbes and plants to potentially increased precipitation in the temperate steppe.

Conclusions/Significance

Increased soil C input and precipitation would show significant effects on soil microbial properties and plant growth in the temperate steppe. These findings will improve our understanding of the responses of soil microbes and plants to the indirect and direct climate change effects.     

短期氮素添加和模拟放牧对青藏高原高寒草甸生态系统呼吸的影响

氮沉降和放牧是影响草地碳循环过程的重要环境因子,但很少有研究探讨这些因子交互作用对生态系统呼吸的影响。在西藏高原高寒草甸地区开展了外源氮素添加与刈割模拟放牧实验,测定了其对植物生物量分配、土壤微生物碳氮和生态系统呼吸的影响。结果表明:氮素添加显著促进生态系统呼吸,而模拟放牧对其无显著影响,且降低了氮素添加的刺激作用。氮素添加通过提高微生物氮含量和土壤微生物代谢活性,促进植物地上生产,从而增加生态系统的碳排放;而模拟放牧降低了微生物碳含量,且降低了氮素添加的作用,促进根系的补偿性生长,降低了氮素添加对生态系统碳排放的刺激作用。这表明,放牧压力的存在会抑制氮沉降对高寒草甸生态系统碳排放的促进作用,同时外源氮输入也会缓解放牧压力对高寒草甸生态系统生产的负面影响。     

The effect of ferrous sulphate on the yield and manganese uptake of oats on sandy soil fertilized with natural pyrolusite

Summary The effects of soil treatments with ferrous sulphate and an equivalent amount of hydroquinone on the yield of dry matter and the manganese uptake of oats were investigated in pot experiments using a sandy soil deficient in manganese, with and without additions of finely ground, natural pyrolusite containing some manganite.In soil not fertilized with pyrolusite an application of hydroquinone gave a higher yield of dry matter and a considerably higher manganese uptake than an application of the equivalent quantity of ferrous sulphate.In soil fertilized with hydroquinone an increase of 23 per cent in the yield of dry matter and an increase of 50 per cent in the manganese uptake per pot were found when the soil was fertilized with 100 g of natural pyrolusite <50µ per pot. In soil fertilized with a quantity of ferrous sulphate equivalent to hydroquinone, an increase of 21 percent in the yield of dry matter and an increase of about 200 per cent in the manganese uptake per pot were found when the 100 g of pyrolusite was applied.     

Development of specific rhizosphere bacterial communities in relation to plant species, nutrition and soil type

Rhizosphere microbial communities are important for plant nutrition and plant health. Using the culture-independent method of PCR-DGGE of 16S rDNA for community analyses, we conducted several experiments to investigate the importance of pH, soil type, soil amendment, nutritional status of the plant, plant species and plant age on the structure of the bacterial community in the rhizosphere. At the same time, we assessed the spatial variability of bacterial communities in different root zone locations. Our results showed that the bacterial community structure is influenced by soil pH and type of P fertilization. In a short-term experiment (15–22 days) with cucumber and barley growing in a N deficient or a P deficient soil, the bacterial community structure in the rhizosphere was affected by soil type and fertilization but not by plant species. In a 7.5-week experiment with three plant species (chickpea, canola, Sudan grass) growing in three different soils (a sand, a loam and a clay), the complex interactions between soil and plant effects on the rhizosphere community were apparent. In the sand and the loam, the three plant species had distinct rhizosphere communities while in the clay soil the rhizosphere community structures of canola and Sudan grass were similar and differed from those of chickpea. In all soils, the rhizosphere community structures of the root tip were different from those in the mature root zone. In white lupin, the bacterial community structure of the non-cluster roots differed from those of the cluster roots. As plants matured, different cluster root age classes (young, mature, old) had distinct rhizosphere communities. We conclude that many different factors will contribute to shaping the species composition in the rhizosphere, but that the plant itself exerts a highly selective effect that is at least as great as that of the soil. Root exudate amount and composition are the key drivers for the differences in community structure observed in this study.     

风速变化对草原生态系统的影响研究进展

在全球风速呈下降趋势的大背景下,研究风速变化对生态系统的影响具有重要意义,尤其是其重要组成部分——草原生态系统。近年来大量学者开始研究风速变化对草原生态系统的影响,主要集中在以下几个方面并得出相关的结论,(1)风速变化会影响植物的生长速率和叶片形态,适当的风速能够促进植物生长发育、提高植被初级生产力,而强风或持续大风不仅会对植物产生破坏作用,还会影响其生长发育;(2)风会最先带走地表细小颗粒,从而导致土壤质地变粗、水分下降、营养成分重新分配;(3)风引起地表边界层和大气边界层物质和能量的转移和交换,热量和水汽的交换导致地表微气候发生变化,如风速降低会导致地表温度升高;(4)风力作用使得土壤水分亏缺、营养成分变化,导致草原生态系统结构变化、草地覆盖度降低、物种生活型复杂化、耐旱植物增加;(5)大气稳定性、CO2交换速率和碳排放都会随着风速的增加而增加,碳吸收则相反,碳通量也因此发生变化。综上,风速降低对于草原生态系统的影响复杂且利弊相当,未来的发展趋势会更加侧重于以下几个方面的发展:研究对象的多样化、加强控制实验的定量化研究、综合多要素的相互作用机理研究、整体结构和功能性的研究。     

地木耳对蕃茄生长的影响

地木耳是蓝藻门植物,具有生物固氮作用,分别以地表施加、土中施加、浸泡材料与酶提取液的方式在番茄的营养生长期和花蕾期施加,均有增肥效应。地表施加效果最好,且营养生长期施加的作用大于花蕾期;地木耳的用量随每一植株生活的环境不同而异。只要使地木耳保持活力,白天进行光合作用,夜间便可进行固氮作用,它可以持续地进行生物固氮,且具有累加效应。     

Preface

Biological properties of soil are not only essential for the maintenance of soil fertility and the sustainability of the plant-soil ecosystems, but also indicators of land reclamation of contaminated or disturbed soils. This experiment involves two plants (barley and field pea) growing in four soils with different hydrocarbon contents. The objective was to study the effect of hydrocarbons on plant growth and microbial activity, and to evaluate the acid phosphatase activity as an indicator of reclamation of hydrocarbon-contaminated soils. Barley root mass decreased with the increase of the hydrocarbon content but field pea roots were not sensitive to the hydrocarbon content in this experiment. The hydrocarbon contamination reduced the plant growth but increased the microbial activity. The acid phosphatase activity was controlled by both plant root production and microbial activity, therefore it was not a good indicator of the reclamation of oil-contaminated soils.