植物提取物、碳酸钠和碳酸氢钠室内对杨树溃疡病菌生长的抑制作用

 采用菌丝生长速率法用金银花的花、黄花蒿的地上部分、蓝桉果实和黄柏果实的乙醇提取物及其不同极性的组分对杨树溃疡病菌菌丝生长的抑制作用进行了测定。以黄柏果实的抗菌活性最强,其次是金银花的花。抗菌活性成分主要存在于金银花的正丁醇组分、黄花蒿的石油醚组分和乙酸乙酯组分、蓝桉的水部分、黄柏的正丁醇组分。当培养基中碳酸钠和碳酸氢钠的浓度分别为8g/L时(对应的pH值分别为10.24和7.71),菌丝生长抑制率分别为100.00%和79.68%。如果用1mol/L氢氧化钠溶液调节培养基的pH值至10.00,菌丝生长抑制率为40.58%。说明碳酸钠或碳酸氢钠对菌丝生长的抑制作用,一方面是由于改变了培养基的pH值,另一方面可能是由于碳酸根和碳酸氢根离子抑制了菌丝的生长。     

碳酸钙和根际作用对酸性红壤解磷微生物丰度的影响

选用玉米品种郑单958为试验材料,设置不添加碳酸钙(CK)、每千克土添加0.3g碳酸钙(Ca-0.3)和0.5g碳酸钙(Ca-0.5)3个碳酸钙处理,以相应处理未种植物土壤为非根际对照土壤,研究了碳酸钙和根际作用对酸性红壤磷酸酶活性及解磷微生物相关功能基因phoC和phoD丰度的影响。结果表明:碳酸钙添加能有效改善玉米生长,促进地上部氮、磷、钾和钙的吸收。土壤酸性磷酸酶(ACP)活性显著高于碱性磷酸酶(ALP)活性,表明酸性土壤中ACP在矿化有机磷方面占主导地位。根际土壤ACP、ALP活性和phoD基因拷贝数均显著高于非根际,而仅Ca-0.5处理ALP活性和phoD基因拷贝数显著高于CK,说明根际效应强于碳酸钙处理。phoC基因拷贝数与土壤铵态氮、硝态氮含量存在显著相关性,ALP活性和phoD基因拷贝数与土壤pH及铵态氮、硝态氮、有效磷、交换性钙含量均存在显著相关性。可见,碳酸钙和根际作用均影响酸性土壤解磷微生物功能和丰度,但根际效应更加明显,这些作用与土壤理化因子的改变密切相关。     

水流近壁面水力剪切力对滴灌系统碳酸钙污垢的影响

针对目前水动力学条件对滴灌系统碳酸钙污垢形成的影响及适宜的污垢控制阈值尚不明确的问题,该研究对不同近壁面水力剪切力（0～0.7 Pa）下的滴灌系统附着碳酸钙污垢总量、晶相组成及表观形貌进行了分析。结果表明：不同剪切力显著（P<0.05）影响了碳酸钙污垢的形成,随着剪切力的增大碳酸钙污垢的总量呈现先增高后降低的趋势,最大碳酸钙污垢形成量的剪切力为（0.42±0.02）Pa。剪切力较低（0～0.42 Pa）时,随着剪切力的增大碳酸钙晶体的尺寸逐渐变大,Ca2+和CO32-的碰撞几率增加且晶体成核效率提高,使得碳酸钙污垢总量呈现增加趋势;剪切力较高（0.42～0.7 Pa）时,随着剪切力的增大碳酸钙晶体大小逐渐减小,且晶体由于高剪切力的作用发生破碎和脱落,使得碳酸钙污垢总量呈现下降趋势。建议灌水器流道近壁面水力剪切力控制在0～0.24 Pa和0.65～0.7 Pa,以减少碳酸钙污垢的形成。本文的研究结果可为高抗堵塞灌水器的研发以及劣质水滴灌技术的应用和推广提供支撑。     

肉桂酸催化合成条件的研究

研究了苯甲醛与乙酸酐的物质的量比、反应时间、催化剂种类以及混合催化剂物质的量比对合成肉桂酸的影响。实验结果表明,苯甲醛与乙酸酐的物质的量比为1∶3,反应时间为60 min,反应温度为170℃,催化剂为氟化钠/碳酸钾(其物质的量比为1∶2)时,肉桂酸的产率达76.6%。该工艺降低了反应温度,缩短了反应时间,提高了产率,并且该方法简单,环境污染小,产品纯度高。     

碳酸盐碱度对达里湖瓦氏雅罗鱼耗氧率、氨氮排泄和排氨基因表达的影响

采用封闭流水式呼吸室法,研究了不同浓度碳酸盐碱度(以下简称CA,10、30、50、70、90、110 mmol/L)对体质量为(84.62±6.70)g的达里湖瓦氏雅罗鱼耗氧率、氨氮排泄率、血氨含量及排氨基因Rh家族(Rhag、Rhbg、Rhcg1和Rhcg2)在鳃组织中表达量的影响。结果表明,随着碱度的升高,瓦氏雅罗鱼的耗氧率和排氨率均表现为先下降后上升的趋势,且都显著低于对照组(P0.05)。在CA90时,耗氧率和排氨率均达到最低值,表明CA90可能是达里湖瓦氏雅罗鱼所能承受的最大碱度胁迫。相反,随着碱度的升高,瓦氏雅罗鱼的血氨含量呈现先上升后下降的趋势,在CA90时达到峰值。然而在CA0~50时,瓦氏雅罗鱼血氨含量无显著差异(P0.05),表明达里湖瓦氏雅罗鱼进化出特殊的排氨机制,使其体内能够保持较低的氨氮含量以此规避氨中毒。定量PCR显示,参与氨转运的4种Rh基因在不同碱度处理组均有不同程度的上调表达;其中Rhcg1和Rhcg2在高碱度(CA110)最为显著(P0.05),表明Rhcg1和Rhcg2可能在达里湖瓦氏雅罗鱼高碱胁迫下的排氨过程中发挥重要作用。能量代谢研究(O∶N)发现,在CA0~70时,雅罗鱼无需消耗过多能源物质即可实现高碱度胁迫下的能量需求;而在碱度为90~110时,则主要消耗脂肪和碳水化合物供能,减少蛋白质耗能,以此降低毒氨的产生。依据上述研究结果,深入探讨了达里湖瓦氏雅罗鱼在高碱胁迫下的排氨策略及其可能的生理和分子机制,为推动达里湖瓦氏雅罗鱼在不同类型盐碱水域的增养殖提供科学依据。     

Influence of biomineralization on the physico-mechanical profile of a tropical soil affected by erosive processes

Most of the soils of tropical countries are affected by erosion processes. As a result, much attention has been dedicated to the use of microorganisms to improve the geotechnical properties and stability of soils in the context of “bioengineering”. This work was carried out to analyze the effects of the use of a CaCO₃ precipitating nutrient on native microbiota with the aim of mitigating the erosion processes in a tropical soil profile. We observed that the use of nutrient B4 enabled native bacteria present in the soil to precipitate calcium carbonate, resulting in improvements in the physical, chemical, mineralogical and mechanical properties of the soil, which allowed the mitigation of the erosion processes that characterize the soil profile studied.     

兴安落叶松容器苗化学剪根效果与根生长潜力测定的研究

采用内壁涂有不同浓度碳酸铜的容器培育出兴安落叶松(Larix gmelini(Rupr.)Rupr.)苗木,苗木侧根受碳酸铜的抑制,减小了根系变形的程度。通过对处理苗木根生长潜力的测定表明:碳酸铜浓度为100～150g/L时改变了兴安落叶松容器苗新根的分布状态,根系中、上层的新根数量明显增加,这样的苗木根系更接近自然发育的苗木根系,从而克服了一般容器苗根系易变形的缺点。     

粉煤灰和碳酸钙对As（Ⅲ）污染土壤上小麦产量性状及麦株As含量的影响

随着经济的发展,土壤As污染问题日益严重。采用露天盆栽试验方法,研究了在As（Ⅲ）污染土壤上,添加粉煤灰和碳酸钙对小麦成熟期产量及其性状、小麦根、茎叶和籽粒As含量的影响,并探讨了粉煤灰和碳酸钙对土壤As（Ⅲ）污染修复的有效方法。结果表明,在土壤中添加100g·kg^-1的粉煤灰或1．0g·kg^-1的碳酸钙能使小麦株高、结实小穗数、穗粒数、千粒重和产量增加。与对照相比,在As（Ⅲ）污染土壤上,100g·kg^-1的粉煤灰处理显著地增加了小麦产量（P〈0．05）,极显著地降低了小麦籽粒As含量（P〈0．01）;1．0g·kg^-1的碳酸钙处理极显著地增加了小麦的穗粒数、千粒重和产量（P〈0．01）,显著地降低了根中As含量（P〈0．05）,极显著地降低了籽粒As含量（P〈0．01）。因此,在As（Ⅲ）污染土壤上,添加100g·kg^-1的粉煤灰或1．0g·kg^-1的碳酸钙能使小麦产量升高,籽粒As含量下降,有效地缓解As（Ⅲ）对小麦的毒害。     

Pedogenic carbonate recrystallization assessed by isotopic labeling: a comparison of 13C and 14C tracers

The C isotopic composition (δ¹³C) of pedogenic carbonates reflects the photosynthetic pathway of the predominant local vegetation because pedogenic (secondary) CaCO₃ is formed in isotopic equilibrium with soil CO₂ released by root and rhizomicrobial respiration. Numerous studies show the importance of pedogenic carbonates as a tool for reconstructing paleoecological conditions in arid and semiarid regions. The methodological resolution of these studies strongly depends on the time scale of pedogenic carbonate formation, which remains unknown. The initial formation rate can be assessed by ¹⁴C labeling of plants grown on loess and subsequent incorporation of ¹⁴C from rhizosphere CO₂ into newly formed carbonate by recrystallization of loess CaCO₃. We tested the feasibility of ¹⁴C and ¹³C tracers for estimating CaCO₃ recrystallization rates by simultaneous ¹⁴C and ¹³C labeling and comparison with literature data. ¹⁴C labeling was more efficient and precise in assessing recrystallization rates than ¹³C labeling. This is connected with higher sensitivity of ¹⁴C liquid scintillation counting when compared with δ¹³C measurement by IRMS. Further, assessment of very low amounts of incorporated tracer is more precise with low background signal (natural abundance), which is true for ¹⁴C, but is rather high for ¹³C. Together, we obtained better reproducibility, higher methodological precision, and better plausibility of recrystallization rates calculated based on ¹⁴C labeling. Periods for complete CaCO₃ recrystallization, extrapolated from rates based on ¹⁴C labeling, ranged from 130 (125–140) to 240 (225–255) y, while it was ≈ 600 (365–1600) y based on the ¹³C approach. In terms of magnitude, data from late‐Holocene soil profiles of known age provide better fit with modeled recrystallization periods based on the ¹⁴C approach.