微咸水滴灌条件下沙穴种植的土壤水盐二维空间分布规律

河套灌区重度盐碱土具有结构性差、导水率低的特点,且该地区淡水资源短缺,为提高土壤水入渗性能,合理开发利用微咸水资源,可在滴头下方设置沙穴并利用微咸水灌溉。为探明不同矿化度微咸水滴灌的沙穴种植条件下二维土壤水盐分布规律,采用室内50 cm×50 cm二维土槽模拟试验,设置蒸馏水(0 g/L),2.0,3.0,4.0 g/L 4种不同矿化度处理,试验历时100 h。结果表明:在深度5 cm距滴头两侧15~20 cm及滴头下方25 cm的盐碱土处,土壤含水量较高,沙土土壤含水率随着矿化度的增加而增加,盐碱土土壤含水率随着矿化度的增加呈现先增加后降低的趋势,采用3.0 g/L灌溉水滴灌时,盐碱土含水率最大(变异系数为7.64%),说明利用3.0 g/L微咸水灌溉可有效提高沙穴种植条件下土壤含水率;入渗100 h后盐分主要聚集在滴头下方25~30 cm处,沙穴结构试验中,灌溉水矿化度为4.0 g/L的情况下土壤平均电导率最大(变异系数为50.59%),水平方向盐分淋洗效果优于垂直方向,且灌溉水矿化度越低,淋洗效果越显著,蒸馏水处理脱盐率为13.99%,灌溉水矿化度为2.0,3.0,4.0 g/L时积盐率分别为7.93%,14.57%,30.05%,脱盐半径随矿化度的增大而减小,3.0 g/L与2.0 g/L积盐量差异不显著(P=0.460>0.05),与4.0 g/L处理下积盐量差异显著(P=0.024<0.05)。结合土壤水盐空间分布规律,利用3.0 g/L微咸水可提高盐碱土土壤含水率,控制沙穴种植结构土壤积盐量,提高根系层土壤保水性。     

不同施肥措施及复垦年限下土壤团聚体的大小分布及其稳定性

土壤团聚体的数量和质量直接影响着土壤性质和有机碳固存。研究长期不同施肥措施及复垦年限对采煤塌陷区土壤团聚体的重量分布比例及其稳定性的影响,为该区域的农业生产和土壤质量提升提供科学依据。采集复垦6年和11年定位试验不同施肥处理耕层土样,选取不施肥(CK)、平衡施氮磷钾肥(NPK)、单施有机肥(M)、有机无机肥配施(MNPK)4个处理,利用干筛法和湿筛法获得4种粒径的团聚体/粉黏粒组分(> 2 mm、0.25-2 mm、0.053-0.25 mm和< 0.053 mm),用> 0.25 mm团聚体含量(R_0.25)、平均重量直径(MWD)、团聚体破坏率(PAD)和土壤不稳定团粒指数(E_LT)表示团聚体的稳定性,并测定了土壤有机碳含量。结果表明：复垦年限对土壤团聚体的含量及稳定性影响产生了显著影响。干筛条件下,复垦6年和11年均显著降低了各处理0.053-0.25 mm团聚体和< 0.053 mm组分的含量,降幅分别为68.39%-87.37%、69.63%-78.32%(6年)和90.01%-93.68%、78.29%-83.93%(11年)；湿筛条件下,复垦11年显著提高了各处理> 2 mm团聚体的含量,增幅达473.35%-645.16%,但是显著降低了0.053-0.25 mm团聚体的含量,降幅为43.67%-57.54%。土壤团聚体的稳定性也随着复垦年限的增加而逐渐增强,表现为DR_0.25、WR_0.25和MWD值呈增加趋势,而PAD和E_LT值呈降低趋势。土壤有机碳含量与DR_0.25、WR_0.25、MWD_水稳性呈极显著正相关关系,而它与PAD和E_LT呈极显著负相关关系。本研究表明,该区域连续复垦11年提高了土壤大团聚体的含量而伴随着微团聚体含量的显著减少,导致土壤结构越来越稳定。它对提高采煤塌陷区复垦土壤肥力、改善土壤结构效果最佳。     

Remediation of saline-sodic soil using organic and inorganic amendments: physical,chemical, and enzyme activity properties

Purpose

Crops grow poorly in saline-sodic soils, and the productivity of these soils can be dramatically improved with proper amendments. Current research mainly focuses on either organic or inorganic soil amendments, whereas few studies address options of combining organic and inorganic amendments. The objective of this study was to develop new organic and inorganic soil amendments which can lower the soil pH, replace sodium, and improve soil structure.

Materials and methods

Polyhalite (PL), microporous potassium-silicon-calcium mineral fertilizer (MF), furfural residue (FR), and fulvic acid (FA) were mixed with four different ratios to produce organic and inorganic soil amendments: PLFR, PLFA, MFFR, and MFFA. And their optimum mixing ratios were determined by comparing the potassium, calcium concentrations, and pH of filtrate after dissolution. Then, a leaching experiment was conducted by packing mixtures (mass ratio of soil to amendment = 219:1, equivalent to 13 t/hm²) of the saline-sodic soil with each one of these amendments plus two contrasts, gypsum (GP), and no amendment (CK). And the remediation effect was compared by pH, EC, ESP, texture, organic recombination degree of clay, saturated hydraulic conductivity, water-stable aggregates fraction, and enzyme (urease, alkaline phosphatase, and catalase) activities of soil.

Results and discussion

After four times leaching experiment, soil treated with PLFR had lower pH and 25.86% lower exchangeable sodium than untreated soils. The water-stable small macroaggregate fractions and saturated hydraulic conductivity of the MFFR-treated soils were significantly increased by 133% and 31%, respectively. Also, the total soil and heavy fraction organic carbons of the soils treated with MFFR in addition to its alkaline phosphatase activity were all significantly higher than the other treatments.

Conclusions

The results revealed that MFFR has more potential as a soil amendment to improve soil structure and quality and thus help in the development and use of saline-sodic lands for agriculture.

     

Effect of soil acidification on the growth and nitrogen use efficiency of maize in Ultisols

Purpose

To examine the effect of soil acidification on growth and nitrogen (N) uptake by maize in Ultisols.

Materials and methods

A clay Ultisol derived from Quaternary red earth and a sandy Ultisol derived from tertiary red sandstone were used in this study. A pot experiment was conducted with maize growing in the two Ultisols acidified to different pH values. Urea with ¹⁵N abundance of 10.11% was used to investigate the distribution of N fertilizer between soil and plant. Total N content and ¹⁵N abundance in plant and soil samples were determined by elemental analysis-isotope mass spectrometry.

Results and discussion

Critical soil pHs of 4.8 and 5.0 were observed for maize growing in the clay and sandy Ultisols, respectively. Below the critical soil pH, increasing soil pH significantly increased maize height and the yield of maize shoots and roots (both P < 0.05), but changes in soil pH showed no significant effect on maize growth above the critical soil pH in both Ultisols. Maize growing in the sandy Ultisol was more sensitive to changes in soil pH than in the clay Ultisol. Increase in the pH in both Ultisols also increased N accumulation in maize, the N derived from fertilizer in maize, physiological N use efficiency, and N use efficiency (NUE) by maize. Changes in soil pH had a greater effect on these parameters below the critical soil pH, compared to above. The change in soil pH had a greater effect on N accumulation in maize, the N derived from fertilizer in maize, and NUE in the sandy Ultisol than in the clay Ultisol. The NUE increased by 24.4% at pH 6.0, compared with pH 4.0 in the clay Ultisol, while the NUE at pH 5.0 was 4.8 times that at pH 4.0 in the sandy Ultisol. The increase in soil pH increased the ratio of N accumulation in maize/soil residue N and decreased the potential loss of fertilizer N from both Ultisols.

Conclusions

Soil acidification inhibited maize growth, reduced N uptake by maize, and thus, decreased NUE. To maintain soil pH of acidic soils above the critical values for crops is of practical importance for sustainable food production in acidic soils.

     

Assessment of soil aggregation properties after conversion from rice to greenhouse organic cultivation on SOC controlling mechanism

Journal of Soils and Sediments - Organic manure is beneficial for macro-aggregate formation and soil organic carbon (SOC), but how SOC change in aggregate fractions in time-series is still...     

中国荔枝文化遗产的特点、价值及保护——基于岭南荔枝种植系统(增城)的实证研究

中国是荔枝的原产地,是荔枝产业第一大国,拥有全球最丰富、最优质的荔枝品种。同时荔枝历史上有"百果之王"等美称,是中国文化底蕴最为深厚的果品之一。荔枝文化遗产极具中国特色且拥有全球影响力,对其保护与发展开展研究具有重要意义。本文以中国重要农业文化遗产岭南荔枝种植系统(增城)为案例,采用实地调查、深度访谈等研究方法,对荔枝文化遗产的特点、价值及保护进行了探讨。遗产地荔枝栽培历史悠久,‘挂绿’驰名中外,种质与古树资源丰富,拥有完备的生产技术体系,荔枝文化资源厚重多元。岭南荔枝种植系统(增城)是一个生态、经济与文化价值俱佳,具有南亚热带特色的生产和文化系统,但当前面临着城镇化与现代农业发展的冲击、古荔树保护力度不够、遗产价值认知不足等威胁。提出以下遗产保护与发展的建议:选择山枝与水枝的代表性区域,建设田园空间博物馆;实施古荔树保护工程,强化古树的管理与护养;加大荔枝文化普及力度,提升民众文化自觉能力;以荔枝产业园、特色小镇、果场为重点,推动荔枝产业升级发展。荔枝相关遗产地应联合申报全球重要农业文化遗产,以推动中国荔枝文化遗产的进一步保护与宣扬。     

DNA条形码技术在中药领域的应用

DNA条形码技术可对物种进行快速自动鉴定,具有鉴定准确、结果稳定、操作简便、适用广泛等特点,目前在中药领域应用较多。从DNA条形码技术在中药材鉴定、种植、流通、市场监管、中成药鉴定和药用植物种质资源调查等中药领域的多个方面进行综述,并探讨DNA条形码技术在中药领域的优势和不足,以期为DNA条形码技术在中药领域的研究提供新的思路。     

“森林资源诅咒”的存在性、传导机制及破解对策:综述与展望

文中研究森林资源丰裕度与经济增长的关系，从森林资源诅咒的存在性检验、传导机制和破解对策3个方面对国内外相关文献进行了梳理总结。结果表明:森林资源诅咒研究已经取得了一定成果，但是现有文献对森林资源诅咒现象的实证研究结果不稳定，会因研究对象、时间、样本以及模型和指标选取的不同而变化；现有研究对森林资源诅咒的传导机制缺乏实证检验，在指标选择和模型构建中尚存在许多不足之处。未来研究需要考虑指标筛选的科学性、计量模型的稳健性以及中介和调节效应的引入等；此外，森林资源丰裕度与经济增长之间的关系可能不是线性关系，因此在建立计量模型时应对模型形式进行优化选择。     

Trx-1 over-expression attenuates oxidative stress injury in MPP+ -induced PC12 cells by regulating NF-κB signaling pathway

AIM:To investigate the inhibitory effect of thioredoxin 1 (Trx-1) over-expression on oxidative stress injury in 1-methyl-4-phenylpyridinium (MPP⁺)-induced rat pheochromocytoma PC12 cells by regulating NF-κB signaling pathway.METHODS:The PC12 cells were damaged by treatment with MPP⁺ at 1, 3 and 5 mmol/L, and the optimal concentration of 3 mmol/L was selected. The cell viability was measured by MTT assay. The oxidative stress indexes lactate dehydrogenase (LDH) activity, superoxide dismutase (SOD) activity and malondialdehyde (MDA) content in the cell culture supernatant were detected, and the protein expression of Trx-1 was determined by Western blot. Lentiviral infection with Ad-Trx-1-GFP sequence was used to establish a model of MPP⁺-treated PC12 cells with Trx-1 over-expression. The effects of Trx-1 over-expression on the cell viability, oxidative stress responses and NF-κB signaling pathway were determined by MTT assay, commercial kits and Western blot. The effects of phorbol 12-myristate 13-acetate (PMA), an activator of NF-κB signaling pathway, on the viability and oxidative stress of PC12 cells were observed. The NF-κB signaling pathway inhibitor pyrrolidine dithiocarbamate (PDTC) was used in MPP⁺-treated PC12 cells with Trx-1 over-expression, and the cell viability and oxidative stress responses were measured. RESULTS:The viability of PC12 cells, SOD activity in the supernatant and protein expression of Trx-1 were decreased, while LDH activity and MDA content in the supernatant were increased significantly by treatment with MPP⁺ at 1, 3 and 5 mmol/L. The effect of MPP⁺ at 3 mmol/L and 5 mmol/L was significantly greater than that at 1 mmol/L (P<0.05), and no significant difference between 3 mmol/L and 5 mmol/L was observed (P>0.05). The inhibitory effect of MPP⁺ on the viability of PC12 cells, and the oxidative stress injury and activation of NF-κB signaling pathway induced by MPP⁺ were significantly attenuated by over-expression of Trx-1. The inhibitory effect of MPP⁺ on the viability of PC12 cells and the oxidative stress injury induced by MPP⁺ were promoted by the activation of NF-κB signaling pathway, while the protective effects of Trx-1 over-expression on the MPP⁺-treated PC12 cells were enhanced by the inhibition of NF-κB signaling pathway. CONCLUSION:Over-expression of Trx-1 protects MPP⁺-treated PC12 cells from oxidative stress injury by regulating NF-κB signaling pathway.