Responses of soil extracellular enzyme activities to carbon input alteration and warming in a subtropical evergreen broad-leaved forest

土壤胞外酶来源于土壤微生物、植物和动物, 是土壤生物地球化学过程的积极参与者, 在森林生态系统的物质循环和能量流动过程中扮演着重要角色。为探明土壤胞外酶活性对碳输入变化及增温的响应, 该研究基于长期增温、去除地表凋落物(以下简称去凋)和切根处理的云南哀牢山亚热带常绿阔叶林控制实验平台, 研究了不同处理(对照、去凋、切根、切根并增温)下表层矿质土壤(0-5和5-10 cm)与碳氮磷获取相关的胞外酶活性, 包括多酚氧化酶(POX)、过氧化物酶(PER)、β-葡萄糖苷酶(BG)、β-1,4-N-乙酰氨基葡萄糖苷酶(NAG)和酸性磷酸酶(AP)。结合铵态氮(NH₄⁺-N)含量、硝态氮(NO₃^--N)含量、溶解有机碳(DOC)含量、溶解总氮(DN)含量、土壤含水量(SWC)等相关指标, 探讨凋落物碳输入、根系碳输入和温度变化对土壤胞外酶活性及其生态化学计量特征的影响。研究结果表明: 在对照样方, 除POX外其余酶活性均为0-5 cm层显著高于5-10 cm层。与对照相比, 长期的凋落物去除显著降低了0-5 cm层土壤AP和BG活性, 对NAG、PER和POX活性则无显著影响; 长期切根处理显著降低了0-5 cm层土壤BG活性, 但提高了两个土层PER活性; 长期切根并增温处理显著降低了0-5 cm层AP和BG活性, 对其余酶活性无显著影响。冗余分析结果显示SWC和NH₄⁺-N含量是驱动土壤酶活性变化的重要因子。本研究为该生态系统土壤碳氮磷生物地球化学关键过程对全球变化的响应提供了土壤酶学的依据。     

亚热带常绿阔叶林土壤胞外酶活性对碳输入变化及增温的响应

土壤胞外酶来源于土壤微生物、植物和动物, 是土壤生物地球化学过程的积极参与者, 在森林生态系统的物质循环和能量流动过程中扮演着重要角色。为探明土壤胞外酶活性对碳输入变化及增温的响应, 该研究基于长期增温、去除地表凋落物(以下简称去凋)和切根处理的云南哀牢山亚热带常绿阔叶林控制实验平台, 研究了不同处理(对照、去凋、切根、切根并增温)下表层矿质土壤(0-5和5-10 cm)与碳氮磷获取相关的胞外酶活性, 包括多酚氧化酶(POX)、过氧化物酶(PER)、β-葡萄糖苷酶(BG)、β-1,4-N-乙酰氨基葡萄糖苷酶(NAG)和酸性磷酸酶(AP)。结合铵态氮(NH₄⁺-N)含量、硝态氮(NO₃^--N)含量、溶解有机碳(DOC)含量、溶解总氮(DN)含量、土壤含水量(SWC)等相关指标, 探讨凋落物碳输入、根系碳输入和温度变化对土壤胞外酶活性及其生态化学计量特征的影响。研究结果表明: 在对照样方, 除POX外其余酶活性均为0-5 cm层显著高于5-10 cm层。与对照相比, 长期的凋落物去除显著降低了0-5 cm层土壤AP和BG活性, 对NAG、PER和POX活性则无显著影响; 长期切根处理显著降低了0-5 cm层土壤BG活性, 但提高了两个土层PER活性; 长期切根并增温处理显著降低了0-5 cm层AP和BG活性, 对其余酶活性无显著影响。冗余分析结果显示SWC和NH₄⁺-N含量是驱动土壤酶活性变化的重要因子。本研究为该生态系统土壤碳氮磷生物地球化学关键过程对全球变化的响应提供了土壤酶学的依据。     

十万大山地区典型次生阔叶林土壤微生物数量及酶活性的季节动态

为了评价广西十万大山南麓次生阔叶林土壤质量的变化,该研究以广西十万大山南麓典型季雨林中的次生阔叶林土壤为对象,采用实地调查与实验分析相结合的方法,对其土壤微生物数量和土壤蔗糖酶、脲酶、磷酸酶、过氧化氢酶的季节动态规律进行研究。结果表明:土壤过氧化氢酶、脲酶、蔗糖酶和酸性磷酸酶在垂直分布上均表现为0~10 cm土层高于10~20、20~30 cm土层,差异显著(P0.05);随季节性水热状况的变化,各种土壤酶活性有明显的季节性变化,其中0~10、10~20和20~30 cm土层中过氧化氢酶活性呈双峰模式,高峰出现在春季和秋季;土壤脲酶、酸性磷酸酶活性均呈单峰模式,高峰均出现在夏季;而蔗糖酶活性呈现秋季夏季春季冬季趋势。土壤细菌、放线菌和真菌含量均随着土壤深度的增加而减小,差异显著(P0.05);细菌、放线菌和真菌数量的季节变化大小顺序呈夏季秋季春季冬季的变化趋势。相对于旱季,在十万大山南麓地区,典型次生阔叶林土壤微生物数量及酶活性季节性变化对高温多降水的雨季响应更明显。     

Impacts of land‐use change on nitrogen status and mineralization in the Mulga Lands of Southern Queensland

Abstract: In the semiarid Mulga Lands of southern Queensland soil nitrogen (N) levels have declined after clearance of the native mulga (Acacia aneura F. Muell. ex Benth.) and conversion to grazed buffel grass (Cenchrus ciliaris) pasture. At three mulga sites, declines in soil total N ranged from 14% to 28% in the surface 10 cm of soil. In situ net N mineralization from December 2003 until November 2004 in the surface 10 cm was 49.5 kg N ha^?1 year^?1 in the mulga woodland, 48.2 kg N ha^?1 year^?1 in the young (<5 years old) buffel pasture (previously sown to wheat (Triticum aestivum L.) and 34.6 kg N ha^?1 year^?1 in the old buffel pasture (>20 years). Ammonium‐N was the dominant N pool under mulga in the top 30 cm, while nitrate‐N was dominant under the buffel pastures. Although ammonium‐N under mulga was significantly different to that for 21‐year‐old buffel pasture at all depths, nitrification and net N mineralization were not different between the three land uses at any depth or in the entire 90 cm profile. The Soil Nitrogen Availability Predictor model was used to predict field N mineralization rates for the mulga woodland and 21‐year‐old buffel pasture by using a medium‐term (6‐week) laboratory incubation to establish basal rates of N mineralization. The Soil Nitrogen Availability Predictor overestimated annual net N mineralization in the 0–30 cm depth of mulga by 9% and underestimated it by 28% for the old buffel pasture. The Soil Nitrogen Availability Predictor could be modified further to accurately predict net N mineralization for the mulga woodlands.     

Biological functioning of Brazilian Cerrado soils under different vegetation types

Aims

Over a 2?year period, we compared the soil biological functioning (SBF) of Cerrado physiognomies ranging from grassland-savannic to forest formations, sampling in the middle of the dry and rainy seasons.

Methods

Soil samples were collected at two depths (0 to 5?cm and 5 to 20?cm) under the following physiognomies: Campo Sujo, Cerrado Ralo, Cerrado sensu stricto, Cerrad?o and Mata de Galeria. The SBF was represented by the simultaneous analyses of microbial biomass carbon, soil basal respiration and the activity of enzymes linked to the C, P and S cycles (β-glucosidase, acid phosphatase and arylsulfatase, respectively).

Results

The results demonstrated that Cerrado physiognomies are a major determinant of SBF patterns. The forest-like physiognomies (Mata de Galeria and Cerrad?o) presented the highest biomass and activity compared to the grassland (Campo Sujo) and savanna physiognomies (Cerrado Ralo and Cerrado sensu stricto). These differences were more evident in the topsoil layer (0 to 5?cm), and the seasonal effect on the SBF of the Mata de Galeria and Cerrad?o was more pronounced than on the other physiognomies.

Conclusions

These results provide a benchmark for evaluating changes in SBF and related processes in Cerrado areas due to shifts toward agriculture and cattle production.     

Soil properties and C dynamics in abandoned and cultivated farmlands in a semi-arid ecosystem

Background and Aims

Land abandonment might be an alternative management for restoring soil conditions and C from prolonged cultivation and agricultural practices. In the present study, the influence of 18–22?years of land abandonment on soil properties, C dynamics and microbial biomass was evaluated in closely situated wheat and alfalfa farmlands, and abandoned lands on calcareous soils, Central Iran.

Methods

Soil properties of the 0–15 and 15–30?cm depths from abandoned lands were compared to those from conventionally cultivated lands (i.e., continuous wheat–fallow and alfalfa–wheat rotation) common in calcareous soils of Central Zagros Mountains.

Results

Soil bulk density in the 0–15 and 15–30?cm layers decreased significantly while total porosity increased significantly in abandoned lands. Generally, soil aggregate stability tended to increase within the abandoned fields owing to increased water-stable macro-aggregates. Soil organic C (OC) contents (g kg^?1) and pools (Mg ha^?1) in the 0–15?cm soil layer increased significantly in abandoned lands compared with cultivated lands, with no effect in the 15–30?cm soil layer after 18–22?years of land abandonment, suggesting the restoration of C is pronounced in the upper 0–15?cm soil depth . The total C accumulation in abandoned lands was 7.0?Mg?C?ha^?1 for the entire sampling depth (0–30?cm) over the 18–22?years of land abandonment, which was 26% greater relative to cultivated lands. Carbon mineralization (Cmin) followed a trend similar to organic C, whereas C turnover (Cmin/OC ratio) was slightly greater in wheat fields. However, soil microbial biomass C (MBC) did not vary considerably among the three land uses.

Conclusions

In brief, improvements, albeit slowly, in soil properties of the top layer with the cessation of cultivation indicated that land abandonment may result in enhanced soil C sequestration, and would maintain fertility and productivity of the farmlands of semi-arid climates.     

New Antidiabetic Targets of α-Glucosidase Inhibitory Peptides,SVPA, SEPA,STYV and STY: Inhibitory Effects on Dipeptidyl Peptidase-IV and Lipid Accumulation in 3T3-L1 Differentiated Adipocytes with Scavenging Activities Against Methylglyoxal and Reactive Oxygen Species

Type 2 diabetes mellitus (T2DM) is a multifactorial disease that requires multiple therapeutic strategies for its management. Bioactive peptides with multiple anti-diabetic targets are attractive therapeutic molecules. The present study was conducted to identify additional anti-diabetic targets of α-glucosidase inhibitory peptides, SVPA, SEPA, STYV, and STY. The α-glucosidase inhibitory activity of the peptides was in the order STYV?>?STY?>?SEPA?>?SVPA while molecular docking against human dipeptidyl peptidase IV (DPP-IV) showed that SVPA had the best binding affinity. In contrast, in vitro studies indicated that SEPA had a significantly higher (P?<?0.05) DPP-IV inhibitory activity (IC₅₀?=?5.78?±?0.19 mM) than other peptides. SVPA and SEPA showed mixed inhibition pattern while STYV and STY were uncompetitive inhibitors of the enzyme. IPI (diprotin A), STYV and STY were not cytotoxic while SEPA displayed some cytotoxicity. In differentiated 3T3-L1 adipocytes, SVPA and STYV were found to induce a significant (P?<?0.05) decrease in intracytoplasmic lipid accumulation when added during the differentiation process while STY, GSH and IPI caused significant reduction (P?<?0.05) in the lipid accumulation when added after the differentiation. The SVPA, SEPA and STYV were better scavengers of methylglyoxal than STY but STYV had the best scavenging activities toward reactive oxygen species and nitric oxide. It was concluded that the four α-glucosidase inhibitory peptides including IPI have multiple targets against type T2DM but, overall, of the four peptides evaluated, STYV tends to have better potential for application as a multifunctional anti-diabetic peptide.

     

内蒙古温带草原土壤微生物生物量碳的空间分布及驱动因素

【目的】探索内蒙古温带草原土壤微生物生物量碳的空间分布特征以及驱动因素。【方法】在内蒙古自治区境内沿着年均温、年降水梯度选择17个草原样点,在土壤剖面上分0-10 cm、10-20 cm、20-40 cm、40-60 cm、60-100 cm五层,分别采集土壤样品,测定土壤微生物生物量碳以及主要的环境和生物影响因子,分析不同草地类型以及不同土壤深度土壤微生物生物量碳的差异,探索非生物因子和生物因子对土壤微生物量碳的影响。【结果】草甸草原土壤微生物量碳最高,典型草原次之,荒漠草原最低。在0-10 cm土壤中,草地类型间的微生物量碳变异系数高于草甸草原和典型草原,低于荒漠草原;在0-100 cm土壤中,草甸草原样点间的微生物量碳的变异系数低于典型草原和荒漠草原。土壤微生物量碳与年降水、土壤含水量、粘粒含量、土壤养分元素、地上生物量、地下生物量呈显著正相关,与年均温和土壤p H值呈显著负相关关系。随着土壤深度的增加,土壤微生物量碳显著减少,非生物因子与微生物量碳的相关性减弱,草地类型间以及同一草地类型不同样点间的变异系数增加。0-10 cm土壤微生物量碳与10-40 cm土壤微生物量碳的相关指数高于0.5,与40-100 cm的土壤微生物量碳的相关指数小于0.3。【结论】内蒙古温带草原土壤微生物量碳的垂直分布呈现一定的规律性,且非生物因子对微生物量碳的影响也呈现垂直减弱的规律。     

Carbon Stocks in an African Woodland Landscape: Spatial Distributions and Scales of Variation

Current knowledge of Africa’s carbon (C) pools is limited despite its importance in the global C budget. To increase the understanding of C stocks in African woodlands, we asked how C stocks in soil and vegetation vary across a miombo woodland landscape and to what degree and at what scales are these stocks linked? We sampled along a 5-km transect using a cyclic sampling scheme to allow geostatistical analyses. Soil C stocks in the top 5?cm (12.1?±?0.6?Mg?C?ha^?1 (±?SE)) and 30?cm depths (40.1?±?2.5?Mg?C?ha^?1) varied significantly at scales of a few meters (autocorrelation distance 14?m in 0–5-cm and 26?m in 0–30-cm interval), and aboveground (AG) woody C stocks (20.7?±?1.8?Mg?C?ha^?1) varied significantly at kilometer scales (1,426?m). Soil textural distributions were linked to topography (r ²?=?0.54) as were large-tree AG C stocks (r ²?=?0.70). AG C stocks were constrained to an upper boundary by soil texture with greater AG C being associated with coarser textured soils. Vegetation and soil C stocks were coupled in the landscape in the top 5?cm of soil (r ²?=?0.24) but not with deeper soil C stocks, which were coupled to soil clay content (r ²?=?0.38). This study is one of the most complete transect studies in an African miombo woodland, and suggests that C stock distributions are strongly linked to topography and soil texture. To optimize sampling strategies for C stock assessments in miombo, soil C should be sampled at more than 26?m apart, and AG C should be sampled at more than 1,426?m apart in plots larger than 0.5?ha.     

Rhizospheric soil enzyme activities and phytominimg potential of Aeluropus lagopoides and Cyperus conglomeratus growing in contaminated soils at the banks of artificial lake of reclaimed wastewater

This work investigates the phytoremediation potential of Aeluropus lagopoides and Cyperus conglomeratus, growing indigenously in the vicinity of an artificial lake of reclaimed water in Tabuk, Saudi Arabia . The sampling sites were located at different distances from the wastewater treatment plants. Trace metal contents were higher in roots than shoots in both these plants. Soil urease activity in rhizophere increased linearly along the sampling sites, however, soil alkaline phosphatase and β-glucosidase activities were higher at site 2 but at site 3, the activities of both these soil enzymes reduced. Significant correlations were observed between soil urease activity and the bioconcentration factor (BCF) of Cd, Cu, Pb, and As in A. lagopoides and translocation factor (TF) for all metals in both these plants. Soil β-glucosidase activity was negatively correlated with the TF of Cd, Cu, Pb, and As in A. lagopoides and positively in C. conglomeratus, respectively. Higher BCF of Cd, Cu and Pb than C. conglomeratus and suitable for phytostabilization, however at site 3, C. conglomeratus showed better phytostabilization efficiency for As, as the BCF of As was higher than the A. lagopoides. On the basis of metal accumulation efficiency and rhizospheric soil urease and β-glucosidase activities, A. lagopoides species proved to be a better option for application in phytostabilization strategy than C. conglomeratus plants in the area surrounding the artificial lake of reclaimed water in Tabuk, Saudi Arabia.     

Fine Root and Soil Organic Carbon Depth Distributions are Inversely Related Across Fertility and Rainfall Gradients in Lowland Tropical Forests

Humid tropical forests contain some of the largest soil organic carbon (SOC) stocks on Earth. Much of this SOC is in subsoil, yet variation in the distribution of SOC through the soil profile remains poorly characterized across tropical forests. We used a correlative approach to quantify relationships among depth distributions of SOC, fine root biomass, nutrients and texture to 1 m depths across 43 lowland tropical forests in Panama. The sites span rainfall and soil fertility gradients, and these are largely uncorrelated for these sites. We used fitted β parameters to characterize depth distributions, where β is a numerical index based on an asymptotic relationship, such that larger β values indicate greater concentrations of root biomass or SOC at depth in the profile. Root β values ranged from 0.82 to 0.95 and were best predicted by soil pH and extractable potassium (K) stocks. For example, the three most acidic (pH?<?4) and K-poor (<?20 g K m^?2) soils contained 76?±?5% of fine root biomass from 0 to 10 cm depth, while the three least acidic (pH?>?6.0) and most K-rich (>?50 g K m^?2) soils contained only 41?±?9% of fine root biomass at this depth. Root β and SOC β values were inversely related, such that a large fine root biomass in surface soils corresponded to large SOC stocks in subsoils (50–100 cm). SOC β values were best predicted by soil pH and base cation stocks, with the three most base-poor soils containing 34?±?8% of SOC from 50 to 100 cm depth, and the three most base-rich soils containing just 9?±?2% of SOC at this depth. Nutrient depth distributions were not related to Root β or SOC β values. These data show that large surface root biomass stocks are associated with large subsoil C stocks in strongly weathered tropical soils. Further studies are required to evaluate why this occurs, and whether changes in surface root biomass, as may occur with global change, could in turn influence SOC storage in tropical forest subsoils.

     

黄河三角洲滩地不同造林模式的土壤酶活性

该文对东营市垦利县柽柳(Tamarix chinensis)林、枣(Ziziphus jujuba)园、旱柳(Salix matsudana)林、刺槐(Robinia pseudoacacia)林、白蜡(Fraxinus chinensis)林、桑(Morus alba)园土壤酶活性及其与土壤化学性质和土壤微生物的关系进行了分析。结果表明:在土壤空间上,脲酶和过氧化物酶活性随土层的增加而减小,多酚氧化酶和过氧化氢酶的活性在土层之间变化不明显。过氧化氢酶与脲酶和多酚氧化酶显著相关,脲酶与多酚氧化酶呈负相关。不同造林模式对土壤过氧化氢酶和过氧化物酶影响不大,对脲酶和多酚氧化活性有显著的影响。各种造林模式增加了脲酶的活性,均高于柽柳林;减小了多酚氧化酶的活性,除刺槐林外,均显著低于柽柳林;而造林模式对过氧化物酶和过氧化氢酶的影响较小。土壤酶活性与土壤养分有一定的相关,其中脲酶与全氮、有机质显著正相关,与速效氮正相关;多酚氧化酶与速效钾正相关,而过氧化氢酶与全氮、速效磷和有机质呈负相关,与土壤pH值相关性不显著;与微生物的相关系数不大,其中脲酶与固氮菌、纤维素分解菌显著正相关,与细菌正相关;多酚氧化酶与固氮菌和细菌负相关;过氧化氢酶与固氮菌显著负相关,与纤维素分解菌负相关。脲酶和多酚氧化酶可以作为滩地土壤质量评价的指标。     

Heavy metal accumulation in frogs surrounding an e-waste dump site and human health risk assessment

Abstract

This study was performed heavy metals (As, Cd, Cr, and Pb) in water, soil and frogs around an electronic-waste dump site. The bioaccumulation factors (BAFs) of heavy metals in three frog species and potential human health risks were assessed. Heavy metals were analyzed using inductively coupled plasma-optical emission spectrometry. The Cd and Pb concentrations in water samples and As and Pb concentrations in soil samples from within the e-waste dump site exceeded the standards. The heavy metal concentrations in the muscles of three frog species were as follows: Cr?>?Pb?>?As?>?Cd, and there were no significant differences among frog species except in the case of Pb (p?<?0.05). Only the Cr concentrations exceeded the food quality standards. The relative order of the BAFs for heavy metals in frogs as a result of uptake from the water and soil was Cr?>?As?>?Pb?>?Cd and Cr?>?As?>?Cd?>?Pb, respectively, which indicated that the uptake from water was greater than that from the soil. The assessment of the health risk index and carcinogenic risk (CR) indicated potential human health effects from As, Cr, and Pb via the consumption of frogs.     

秦岭火地塘林区油松(Pinus tabulaeformis)林休眠期的土壤呼吸

林木休眠期林地土壤CO2释放是森林生态系统碳平衡关键组成部分之一.由于绝大多数森林生态系统林木休眠期土壤CO2释放过程测定困难,国内有关林木休眠期CO2释放,量化方面的研究开展较少.采用动态开路气室法对秦岭火地塘林区天然次生油松(Pinus tabulaeformis)林土壤呼吸的日变化进行了测定,分析了土壤呼吸速率(mgCO2m-2h-1)与土壤温度和体积含水率的关系,基于土壤日均呼吸速率和土壤日均温度指数方程与观测季的总天数,估算了林木休眠期林地土壤CO2释放量.结果表明:(1)研究区林地土壤呼吸速率存在较大的时、空变异.不同观测部位土壤呼吸速率的峰值出现时间各异,呼吸作用较弱的时段也不一致.同一观测部位不同观测月中,土壤日均呼吸速率变异系数分别为48.38%,82.51%和81.88%;(2)当土温＞8.5 ℃时,0～5 cm和5～10 cm土层,土壤日均温与土壤日均呼吸速率间存在极显著(p＜0.001)的指数关系,Q10分别为1.297和1.323;(3)0～5 cm和5～10 cm土层,土壤体积含水率与土壤呼吸速率间关系复杂;(4) 林木休眠期研究区林地土壤CO2释放量变化于(977.37±88.43)～(997.19±80.73) gCm-2(p=0.005)间.     

Using hydrogel and clay to improve the water status of seedlings for dryland restoration

The decomposition of soil organic matter is mediated by extracellular enzymes. The aim of this work was to identify the factors determining the activity and size of the mobile fraction of extracellular enzymes (laccase, Mn-peroxidase, endocellulase, cellobiohydrolase, ??-glucosidase, endoxylanase, ??-xylosidase, ??-glucosidase, chitinase, arylsulfatase, phosphatase, phosphodiesterase, alanine and leucine aminopeptidase) using a set of soils covering a wide range of physico-chemical properties. Organic matter content had a major effect on enzyme activity both in forest and grassland soils, while the effects of pH and humic compounds content were only important in forest soils, and the molecular mass of humic compounds and Ca content were only important in grasslands. Specific enzyme activity was either comparable between the soil types or higher in grasslands. With the exception of Mn-peroxidase and ??-glucosidase, the specific activities of all enzymes in arable fields under tillage were similar to those in grasslands. Mobility differed among the enzymes and ranged from <1% for arylsulfatase and phosphodiesterase up to 20?C40% for ??-glucosidase and aminopeptidases, with pH being the most important variable. These results demonstrate that the factors regulating enzyme activity are likely to be different in forest soils and grasslands and that enzyme mobility is a characteristic feature of each individual enzyme.     

桂北不同林龄桉树人工林土壤微生物数量和酶活性特征研究

为探讨桉树不同林龄土壤微生物活性的响应特征,该研究采用时空互代法,选择广西北部低山丘陵地区1～5年生桉树人工林为研究对象,分析了土壤微生物、酶活性在不同土层和季节的变化规律。结果表明:(1)土壤微生物和酶活性在土层中有明显的垂直分布特征,均随土层加深而趋于降低,且各土层间差异显著。(2)细菌、放线菌数量随季节的大小顺序为秋季>夏季>春季>冬季,真菌的变化规律为春季>夏季>秋季>冬季,而酶活性随季节变化表现为夏季、秋季活性较高,春季、冬季活性较低。(3)细菌、真菌、脲酶、过氧化氢酶随林龄增大表现出先减小后增大的趋势,放线菌则呈现先减小后增大再减小的趋势,而蔗糖酶、酸性磷酸酶随林龄的增大趋于增大。(4)林地土壤中三大类群微生物与四种土壤酶之间存在极显著正相关关系,说明土壤微生物与土壤酶活性相互影响,两者之间关系密切,共同影响土壤的质量。综上可知,不同土层土壤微生物和酶活性的季节响应特征差异较大,总体在冬季最低,主要与气温、水分条件、凋落物养分的归还等有关。不同季节、土层、林龄之间的交互作用对土壤微生物和酶活性有显著影响。     

Selenium Accumulation by Brassica Napus Grown in Se-Laden Soil From Different Depths of Kesterson Reservoir

Selenium (Se) may be present in soils and sediments in high concentrations and yet not be mobile or available for plant uptake. Phytoremediation of Se by canola (Brassica napus) was evaluated in sediment from Kesterson Reservoir at three different depths (0 to 30, 30 to 60, 60 to 90?cm) under greenhouse and field conditions. In the greenhouse study, total soil Se concentrations at preplant ranged from 10 to 112?mg kg^?1. Shoot Se concentrations of canola were 182, 53, and 19?mg kg^?1 DM in the 0 to 30, 30 to 60, and 60 to 90?cm depths, respectively. Percentages of Se accumulated by canola relative to total Se loss in the soil at postharvest were as high as 24%. In the field study, total soil Se concentrations were as high as 26?mg kg^?1 soil. Field-grown canola accumulated approximately 50?mg kg^?1 DM, which accounted for less than 10% of total Se lost in the soil at postharvest. Phytoremediation of Se-laden soils under field conditions was about 50% of that observed under controlled greenhouse conditions. This relationship may be useful for prediction of field remediation operation using greenhouse generated data.     

Proline improves copper tolerance in chickpea (Cicer arietinum)

The present study suggests the involvement of proline in copper tolerance of four genotypes of Cicer arietinum (chickpea). Based on the data of tolerance index and lipid peroxidation, the order for copper tolerance was as follows: RSG 888?>?CSG 144?>?CSG 104?>?RSG 44 in the selected genotypes. The basis of differential copper tolerance in chickpea genotypes was characterized by analyzing, antioxidant enzymes (superoxide dismutase, ascorbated peroxidase and catalase), phytochelatins, copper uptake, and proline accumulation. Chickpea genotypes showed stimulated superoxide dismutase activity at all tested concentrations of copper, but H₂O₂ decomposing enzymes especially; ascorbate peroxidase did not increase with 25 and 50 μM copper treatments. Catalase activity, however, increased at lower copper concentrations but failed to stimulate at 50 μM copper. Such divergence in responses of these enzymes minimizes their importance in protecting chickpea against copper stress. The sensitive genotypes showed greater enhancement of phytochelatins than that of tolerant genotypes. Hence, the possibility of phytochelatins in improving copper tolerance in the test plant is also excluded. Interestingly, the order of proline accumulation in the chickpea genotypes (RSG 888?>?CSG 144?>?CSG 104?>?RSG 44) was exactly similar to the order of copper tolerance. Based on hyperaccumulation of proline in tolerant genotype (RSG 44) and the reduction and improvement of lipid peroxidation and tolerance index, respectively, by proline pretreatment, we conclude that hyperaccumulation of proline improves the copper tolerance in chickpea.     

Species Trials of Short Rotation Woody Crops on Two Wastewater Application Sites in North Carolina,USA

Forty-two Populus spp. clones, Eucalyptus benthamii, and seven tree species native to North Carolina were evaluated for survival and height growth through the establishment phase at two municipal wastewater application sites. Groundwater was monitored at each site to determine if establishment of the species trials resulted in exceedances of nutrient mitigation requirements. At the Gibson Wastewater Treatment Facility, 26 Populus clones had 100 % survival, with mean height growths ranging between 152 to 260 cm, and basal diameters ranging between 11.4 and 28.8 mm. Green ash, planted in 2011 and 2012, had high survivorship (>95 %) with first year mean height growth of 30?±?28 cm (2012) and second year mean height growth of 101?±?52 cm (2011). Basal diameter for green ash was 33.3?±?12.6 mm. E. benthamii had moderate survivorship (>77 %) and first year mean height growth of 47?±?27 cm. At the Jacksonville Wastewater Treatment Facility, green ash and bald cypress had high survivorship (>96 %), first year mean height growths of 14?±?25 cm and 27?±?16 cm, and basal diameters of 13.1?±?3.9 mm and 11.6?±?4.8 mm, respectively. Survivorship for 12 Populus clones ranged from 50 and 94 % with mean first year height growths between 58 to 121 cm, and basal diameters between 6.8 and 12.5 mm. E. benthamii had low survivorship (43 %) with mean first year height growths of 17?±?17 cm and basal diameters of 12.0?±?7.7 mm. Groundwater concentrations of NO₃?+?NO₂ and N-NH₄ remained below regulatory requirements at both sites with one exceedance in February 2012 in Jacksonville, NC. The results show that some Populus clones are excellent candidates for woody biomass production on municipal wastewater application fields. Native green ash and bald cypress are also good candidates, but these trees may require longer rotations than Populus to achieve similar biomass yields.