应用暗沟排水技术改良陕南冬水田的效果

在陕南30余万亩冬水田中,有灌溉水源保证和自流排水条件,可以实行暗沟排水的约18万余亩。几年来的试验表明,将田间的固定性主沟修成暗沟后,其增产幅度均远高于明沟改良区和垄畦栽培区。通过定位观测,初步确定了暗沟的规格、深度和间距。改良后,土壤的结构和孔隙状况明显改善,氧化还原电位大幅度升高,有效养分供应也逐渐增强。     

Olive mill wastewater irrigation of maize: Impacts on soil and groundwater

The environmental impact of irrigating a maize field with weathered olive mill wastewater (OMW) for 5 years was assessed. The use of the weathered OMW added the following concentrations of nutrients to the field: 11.8 t/ha/yr carbon, 1033 kg/ha/yr total nitrogen, 23.8 kg/ha/yr phosphorous and 4161 kg/ha/yr potassium. The maize field received 6 times more nitrogen, 50 times more potassium and 2 times less phosphorous than the recommended fertilization rates. The presence of carbon increased microbial activity for organic nitrogen breakdown and the decomposition rate of organic nitrogen. No significant increase was observed of heavy metal accumulation in the soil. Electrical conductivity in the soil remained below the salinization threshold. No direct exposure values were exceeded. No impact on groundwater quality was observed. Irrigation of crops like maize with weathered OMW could be part of a viable decentralized solution for olive mill wastewater use in areas with low organic matter and high irrigation demand.     

水溶性聚丙烯酸纳低聚体的合成

该文论述了以丙烯酸钠为单体，采用氧化还原引发剂，通过调节聚合的方式合成聚丙烯酸钠低聚物。并对单体浓度、引发剂用量、溶液的ｐＮ值、分子量调节剂用量对聚合反应速率、转化率及聚合物平均分子量的影响等进行了详细的讨论。     

质膜氧化还原系统在植物伸长生长中的作用

以大豆下胚轴切段为材料，研究了质膜氧化还原系统对其伸长生长的作用，结果表明，ＮＡＤＨ氧化酶活性与大豆下胚轴伸长生长相关性极显著（Ｒ＝０．９４，Ｐ＝０．０１），而ＮＡＤＨ－Ｆｅ（ＣＮ）３－６氧化还原酶活性与其相关性不显著。大豆下胚轴伸长生长最快的第一切段，其ＮＡＤＨ氧化酶活性最高。第一切段的伸长生长及ＮＡＤＨ氧化酶对ＩＡＡ均有明显的正负反应。ＩＡＡ促进ＮＡＤＨ氧化酶活性。生长延缓剂Ｂ９对第一切段的伸长生长及ＮＡＤＨ氧化酶活性有抑制作用     

禾本科秸秆对植烟土氧化还原电位和营养效率的影响研究

选择3种植烟土壤(酸性、中性及偏碱性),设置禾本科秸秆与化肥配施,单施化肥等处理,通过对植烟土壤根区氧化还原电位(Eh)的原位测定,研究施用有机物对植烟土壤根区Eh、烤烟吸收矿质营养效率和烟叶质量等的影响。结果表明:配施秸秆能提高土壤根区的Eh,显著增加烤烟的营养效率吸收以及增加烟叶的产量和产值。     

Redox condition and nitrate change in a newly flooded rice soil under percolation as influenced by oxidative iron and manganese

Nitrate leaching from intermittently flooded rice fields contributes to nitrate pollution in groundwater. In this study, redox conditions and nitrate change in a newly flooded rice soil under the influence of oxidative iron (Fe) and manganese (Mn) were investigated using flooded soil columns under moderate percolation (4.2?mm?d^?1). The amendments of α-Fe₂O₃ and β-MnO₂ powder (5 and 2.7?mg?g^?1, respectively) delayed the establishment of reducing conditions and lowered the rate of nitrate removal in the soil column, and subsequently increased the percolation of soil indigenous nitrate (8.3?mg nitrogen [N]?kg^?1) from 2.0% to 8.0%, and the percolation of externally amended nitrate (250?mg?N?kg^?1) from 11.0% to 26.0%. The pool of oxidative iron-centered metal oxidants needs to be jointly considered with the availability of organic carbon and hydrological conditions in evaluating redox conditions and nitrate change in intermittently flooded rice soils.     

Effect of water management on the vivianite content of paddy-rice roots

Abstract

Vivianite is a hydrated ferrous phosphate mineral that can form in reducing environments, and it was recently identified on aged paddy rice (Oryza sativa, L., cultivar Hitomebore) roots. However, the formation and dissolution of vivianite appear highly susceptible to the soil redox potential. We examined the effect of water management on the vivianite content of rice roots in three experimental micro (1 m²) paddy fields. The vivianite content of the roots was estimated using a method based on the alteration of vivianite after heating at 105°C for 48 h. This alteration steeply lowers the dissolution of phosphate from the roots in a mixed acid solution of 0.1 mol L^?1 of hydrochloric acid (HCl) and 1 mol L^?1 of acetic acid (CH₃COOH). Efficiency of the method was confirmed regarding heating temperature and duration of heating. Using this method, we found that water management significantly influenced the vivianite content of the rice roots. The vivianite content of the rice roots was highest, i.e., 2.3 g phosphorus (P) kg^?1 expressed by its estimated P content, when the paddy field was continuously flooded from May to until early September. After flooding stopped, the soil was gradually oxidized, leading to a decrease in vivianite content. In the micro plot exposed to midseason drainage, the vivianite content increased to the level of the continuously flooded plot after reflooding, and finally decreased after flooding was stopped in late August. The plots exposed to midseason drainage followed by intermittent irrigation presented the lowest vivianite contents among the three experimental paddy fields. These results confirm that increases and decreases in the vivianite contents of paddy-rice roots strongly depend on water management.     

Elemental affinity for siderite found in a Japanese paddy subsoil

ABSTRACT

Siderite (FeCO₃), a type of carbonate mineral, is very occasionally recognized as a nodule in anoxic soils and sediments. During siderite formation, elements are expected to be accumulated or excluded between siderite and bulk soil. Therefore, we verified the affinity of 40 elements for siderite found in the gley horizon of a smectite-rich paddy field in northeastern Japan from the elemental concentration of the soil and the siderite dissolved in 2.88 mol L^?1 hydrochloric acid (10% HCl). The concentration ratio of the target element of the soil to the siderite was expressed by the product of the dimensionless R₀ value and ratio of titanium (Ti) concentration of the soil to the siderite (C_siderite /C_soil) = R₀ (Ti_siderite /Ti_soil). The affinity of each element for the siderite was analyzed by comparing the R₀ values. In comparison with Ti used as the reference element, P, Cr, Co and Mo were accumulated (R₀ > 1.0), and alkali metals, such as Li, Na and K, and chalcophile elements, such as Cu, Zn, Cd and Pb, tended to be equal or excluded from the siderite (R₀ ≦1.0). Of the group 2 elements, Ca, Sr and Ba were accumulated, while Mg was excluded. The affinity of Mn for siderite exceeded that of Fe as the main component of the siderite, which reflects the fact that siderite was formed in a fresh water condition. The siderite size did not influence the elemental affinity. Observation of micromorphology using a scanning electron microscope showed that the siderite nodules were aggregations of siderite particles and clays, suggesting that the siderite grew by taking in clay around it. The rare earth element (REE) distribution pattern showed a tendency not to increase linearly but to increase with forming a concave curve at the intervals of the four elements with the increase of atomic number (i.e. tetrad effects). Although these findings are from the lower horizons of anoxic soils, the elemental affinity for siderite of this study is useful in order to elucidate the complex elemental dynamics in the anoxic environment.     

Behavior of iodine in a forest plot,an upland field and a paddy field in the upland area of Tsukuba,Japan: Seasonal variations in iodine concentration in precipitation and soil water and estimation of the annual iodine accumulative amount in soil horizons

Abstract

In the course of a series of studies conducted to investigate the long-term behavior of ¹²⁹I (which has a half-life of 16 million years) in the environment, seasonal variation in the concentration of stable iodine (¹²⁷I) in precipitation and soil water to a depth of 2.5 m in a forest plot, an upland field and a paddy field in the upland area of Tsukuba, Japan, were determined. Iodine concentration in precipitation tended to increase during the summer (high air temperature) season and low-rainfall period, and a positive high correlation was observed between annual rainfall and the annual amount of iodine supplied by precipitation. No seasonal variations in iodine concentration in soil water were observed at any depth in the forest plot and upland field unlike at shallow depths (0.2 and 0.5 m) in the paddy field. In the paddy field, from the beginning of summer irrigation, under flooding conditions, iodine concentration in soil water at shallow depths (0.2 and 0.5 m) continuously increased, and immediately before mid-summer (intermittent) drainage and drainage, the maximum iodine concentration (approximately 50 µg L^?1) and lowest E_h values (approximately ?150 to ?200 mV) were recorded. These high iodine concentration levels and low E_h values were ascribed to high air temperature (approximately > 25°C on average every 10 days) and the continuation of the groundwater level above the ground surface. As for the temporary winter irrigation period (mean daily air temperature 2?4°C), the iodine concentration was low (1.7–3.7 µg L^?1) at all depths, as was the case in the non-irrigation period. After mid-summer drainage, and drainage, the iodine concentration in soil water at depths of 0.2 and 0.5 m decreased drastically as the groundwater level decreased. The mean annual amount of iodine accumulated in the surface soil horizons (0–0.67 m) in the forest plot was estimated to be approximately 2.9 mg m^?2 (7.5 µg kg^?1 dry soil), which coincided with the mean annual amount of iodine supplied to the earth surface by precipitation. A mildly oxidative subsurface 2Bw horizon (0.60–0.89 m) in the paddy field was estimated to illuviate approximately 3.1 mg m^?2 (20 µg kg^?1 dry soil) of iodine annually by retaining iodine in the soil water percolated to this horizon.