共查询到20条相似文献，搜索用时 187 毫秒
1.
通过实地调查,研究了江苏省22个典型茶园表层土样和12个剖面土样的全硒含量,分析了土壤全硒含量分布特性、有效硒含量及其影响因素。结果表明,江苏省典型茶园土壤全硒含量在0.10～1.78mg·kg-1之间,平均为0.50mg·kg-1,高于全国平均值。其中,宜兴地区土壤全硒平均含量为0.88mg·kg-1,明显高于其他地区的0.25mg·kg-1,但前者土壤硒活化率仅为4.94%,明显低于江苏省平均值9.04%。宜兴地区虽然土壤供硒潜力巨大,但要充分利用富硒土壤开发、生产富硒茶必须提高土壤中硒的活化率和可利用度。土壤有效硒与土壤pH值、CEC呈极显著正相关,在实际生产中可通过提高土壤pH值等改善土壤环境条件的方法来提高土壤硒的有效性,从而提高茶叶中硒的含量。研究区内硒在表层土壤中的相对含量趋向增加,生物积累大于淋溶作用。 相似文献
2.
进行土壤硒分布及其影响因素研究,对掌握区域硒空间分布现状、区域农产品安全以及人体健康具有重要意义。在遵义市采集了701个表层土壤样本,分析了样品中的硒含量。利用GS+软件构建半变异函数模型,采用克里格法预测了遵义市土壤硒含量空间分布特征,并进一步探讨土壤pH值、全氮、有机质、海拔高度和成土母质等因素对硒含量及其空间分布的影响。结果表明:遵义市土壤硒含量变幅为0.10～2.90 mg·kg~(-1),平均值为0.56 mg·kg~(-1),总体上处于足硒和富硒土壤范畴,缺硒与少硒土壤较少,西北部和南部边缘存在明显的土壤富硒带,中部和东部地区土壤硒含量较低。土壤硒含量与pH值无相关关系,与土壤全氮、有机质和海拔高度呈显著正相关关系。此外,遵义市富硒岩层和广泛出露含硒量高的煤矿层可能也是影响土壤含硒量的主要因素。 相似文献
3.
基于香港地区51个剖面土壤和44个表层土壤中总硒量的分析,对香港土壤硒含量、分布及其影响因素进行研究.分析结果表明,香港土壤总硒量变幅在0.07～2.26 mg kg-1,平均含量为0.76 mg kg-1,在湿润铁铝土中的硒含量最高,平均为1.05 mg kg-1,含量最低的为旱耕人为土,平均为0.45 mg kg-1;在土壤剖面中硒主要分布在心土层和底土层.林地土壤硒含量(1.36 mg kg-1)较高, 农业土壤较低(0.36 mg kg-1).影响香港土壤硒含量及其分布的因素主要是成土母质.土壤pH值、有机质、粘粒和Fe、Al的含量也是影响土壤硒富集与分布的因素. 相似文献
4.
为了解清镇市土壤硒(Se)含量特征与空间分布,明确其背景值与基准值,探明成土母岩、表生环境(土壤酸碱度、有机质、土壤类型等)与人类活动(施肥、浇灌等)对土壤Se含量的影响,采集了清镇市表层(0～20 cm)土壤样品4 637件和深层(150～200 cm)土壤样品216件,分析了土壤p H、有机质、Se含量等指标。结果表明：清镇市表层土壤Se含量高于深层土壤,表层与深层土壤Se含量空间分布趋势一致;Se含量较高的区域集中分布在流长苗族乡、犁倭镇与站街镇接壤的区域;清镇市富硒(0.4～3.0 mg/kg)土壤面积为103 789.65 hm2,占调查总面积的89.98%;清镇市土壤Se背景值为0.56 mg/kg,土壤Se基准值为0.35 mg/kg,该背景值是全国土壤Se背景值的1.93倍,且高于贵州省土壤Se背景值。清镇市不同土地利用方式与黄壤、黄棕壤、石灰土和水稻土的土壤Se背景变化率(ΔRCSe)均增加。2009—2019年清镇市土壤p H降低了0.15个单位,表层土壤Se含量与pH负相关,与有机质和深层土壤Se含量正相关,Se元素更容易在酸性强、有机质丰富... 相似文献
5.
大庆龙凤湿地土壤理化性质与硒元素分布关系研究 总被引：5，自引：0，他引：5
为了解大庆龙凤湿地土壤理化性质对硒的含量、形态与分布的影响,对大庆龙凤湿地保护区4个样区20个样点4个不同层次土样中硒的含量、形态、分布以及部分理化性质进行了研究。结果表明:大庆龙凤湿地土壤全硒含量为121～150μg/kg,由于硒淋溶流失的影响,随土壤深度的增加,全硒含量无明显变化;有效硒总量为22～28μg/kg,包括水溶态硒、交换态硒与富啡酸态硒三种形态。影响土壤硒的主要因素包括土壤有机质、土壤黏粒含量及pH值,其中土壤有机质、黏粒含量与硒含量之间存在正相关关系,土壤pH值与硒含量存在极显著的负相关关系。 相似文献
6.
赣南地区设施菜地土壤全硒含量分布特征 总被引：1，自引：1，他引：0
为探究江西省赣州设施菜地土壤全硒（Se）的含量及其分布特征,于2021年对赣南地区设施蔬菜大棚采集0～20 cm耕层土壤样235件,测定了土壤采样点的经纬度、海拔及土壤中全硒含量和理化性质。结果表明,赣南地区设施菜地土壤全硒质量分数平均为0.31 mg/kg,变化范围为0.03～1.25 mg/kg,全硒含量分布频率符合正态分布。研究区域设施菜地富硒土壤资源较为丰富,85.1%的样点数土壤全硒含量处于足硒及以上水平（>0.175 mg/kg）,其中有22.1%的样点数土壤属于富硒水平标准（>0.400～3.000 mg/kg）,而富硒土壤主要集中在赣南地区的正西部及东北部等部分区域;7.2%和7.7%的样点数土壤全硒质量分数分别达硒不足（>0.125～0.175 mg/kg）和潜在硒不足水平（≤0.125 mg/kg）,二者主要集中在赣南地区西南角部分区域,不存在硒中毒区域。海拔每增加1 m,设施土壤全硒质量分数降低5.35×10-4 mg/kg;纬度每增加1°和pH值每增加一个单位,土壤全硒质量分数分别增加0.090和0.049 mg/kg。综上,赣南地区设施菜地土壤硒资源具有较大利用潜力,并可依据研究区域全硒含量分布特征开展具有针对性的设施富硒蔬菜发展策略。 相似文献
7.
以大巴山区典型早古生代地层上发育的自然土壤为对象 ,研究了大巴山区土壤中Se、F等生命元素的含量及分布规律。结果表明 :大巴山区土壤中硒、氟的平均含量分别为 6 65± 14 2 5μgg- 1和 670±451μgg- 1,远高于对照和中国土壤背景值 ;富Zn贫Fe的土壤环境有利于Se、F的富集 ;土壤中硒、氟的含量受地层分布、母岩岩性等因素的控制 ,同时 ,表生地球化学作用、生物作用以及山地剥蚀地貌也影响它们在土壤中的重新分配。 相似文献
8.
张宣葡萄产区土壤硒含量与葡萄品质关系研究 总被引：1，自引：0，他引：1
调查分析了张宣地区葡萄园产区土壤硒分布状况,并与葡萄品质进行了相关分析,结果表明:张宣葡萄产区表层土壤硒含量低于中国表层土壤硒含量,在怀涿葡萄产区总面积占67.74%的土壤属于缺硒土壤,24.73%产区土壤为少硒土壤,足硒土壤面积较少;宣化葡萄产区面积达81.82%产区土壤为足硒土壤;土壤硒含量与土壤有机质含量呈极显著正相关,与土壤pH呈极显著负相关,偏相关分析显示该产区土壤有机质与土壤硒含量的关系更密切;土壤硒含量与葡萄果实Vc有负相关关系,与果实中pH、单粒重呈正相关关系,分析表明土壤硒与酿酒葡萄品质关系密切;土层深度在土壤硒含量与葡萄品质的关系中影响不大。 相似文献
9.
贵州开阳地区新元古代灯影组白云岩风化成土剖面微量元素地球化学特征 总被引：1，自引：0，他引：1
硒是人体必需的微量元素,土壤中的硒含量受基岩的控制,研究土壤中硒的分布情况,对合理开发利用土地资源具有重要意义。通过对开阳地区红粘土剖面的结构、颜色、微量元素、稀土元素分布特征研究,提出红粘土层可划分为两层:底部为暗紫褐色粘土,含有很高的Se元素及其它微量元素和稀土元素;顶部为紫红色粘土-灰黄色粘土,Se元素以及其它微量元素、稀土元素含量较低。基岩是红粘土剖面中硒元素的物质来源,其是土壤中硒含量的主要控制因素,另外,Fe含量、pH值、有机质也是微量元素包括硒元素、稀土元素富集的重要的控制因素,硒元素在铁质层和红粘土底部超常富集,这两层中硒含量分别是中国土壤硒平均含量的14.35倍和34.78倍。 相似文献
10.
滕州表层土壤硒异常特征及来源分析 总被引：1，自引：1，他引：0
为确定影响滕州地区表层土壤硒含量变化的因素,对研究区土壤的地球化学指标进行统计分析,结果显示,研究区土壤硒背景值为0.08mg/kg,异常下限值为0.17 mg/kg,表层土壤硒平均含量为0.23 mg/kg,标准差为0.144 mg/kg,变异系数为62.6%。综合相关性分析、主成分分析以及富集因子分析结果,表明表层土壤硒异常主要受人为因素的影响。不同区域表层土壤硒含量由高到低依次为煤矿区交通繁忙区农田区。在土壤垂直方向上,煤矿周边土壤中硒含量自下而上增加的趋势要明显快于不受煤矿直接影响的区域,同时前者的变化速率和转折端的出现均快于后者。因此,滕州地区表层土壤硒异常主要受煤矿开发的影响。 相似文献
11.
黔中地区水稻土的含硒量及其对糙米硒含量的影响 总被引：7，自引：0，他引：7
通过贵州开阳县水稻土硒含量特征和该区水稻硒含量之间关系的调查研究表明:开阳县水稻土水溶性硒含量高于一般水稻土水溶性硒的临界值(0.01μgg-1),这与该区的成土母质、地形等因素有关。富硒水稻土使水稻对硒的吸收增加,该县出产的稻米硒含量普遍比贵州省其它地区高,平均含硒量高于粮食硒的正常含量范围(0.04~0.07μgg-1)。水稻地上各部分含硒量存在差异,糠、秸秆中的含硒量高于糙米,糙米含硒量与土壤硒含量的相关性达极显著水平(r=0.7861*,P<0.05)。 相似文献
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13.
Tokunaga Tetsu K. Lipton Douglas S. Benson Sally M. Yee Andy W. Oldfather Joan M. Duckart Eugene C. Johannis Paul W. Halvorsen Kathleen E. 《Water, air, and soil pollution》1991,(1):31-41
Kesterson Reservoir, in the San Joaquin Valley of California, was used for disposal of saline, seleniferous agricultural drain waters during the years 1981 - 1986. The combined effects of infrequent drain water application, reduction and oxidation of Se, and evapotranspirative removal of soil water within the upper 1 m of the soil profiles appear to provide explanations for distribution patterns of Se in soils of upland sites. From 1987 to 1990, an approximate doubling in average soil solution Se concentrations was observed. It is shown that currently only relatively insignificant quantities of Se have been transported into the Pond 11 soils from the shallow water table. Sequential extraction of these upland soils indicated that substantial inventories of Se were associated with soluble, adsorbed, carbonate, and soil organic matter fractions, while Se retained within refractory inorganic fractions were minor. The mobilization of Se from these potentially labile pools may account for the observed increases in soil solution concentrations of Se following the draining of Kesterson Reservoir. 相似文献
14.
Moustafa A. Elrashidi 《Communications in Soil Science and Plant Analysis》2018,49(9):1083-1091
Selenium (Se) is an essential micronutrient for humans and animals and can be toxic when present in high concentrations in soil and water. Many soils in Gunnison and Uncompahgre River Basins in West-Central Colorado are formed from deposits derived mainly from weathered Mancos shale that have high concentration of Se and salts. Elevated concentrations of Se and salts were detected in streams and rivers in this area. The objectives were to determine the amount and distribution of different forms of Se and relationships with physical and chemical properties for soils derived from Se-rich Mancos shale. The information may help to improve land management practices and minimize the environmental impact on natural water resources. A total of 48 topsoil samples and soils from horizons in 9 pedons were investigated. The total and water-soluble Se and other elements as well as physical and chemical properties were determined in soils. The total Se ranged from 330 to 5,673 µg/kg with a mean of 2,224 µg/kg. The water-soluble Se ranged from a minimum of 4.95 µg/kg to a maximum of 2,415 µg/kg and a mean of 338 µg/kg. A highly significant correlation was detected between the total and water-soluble Se in soils. Both the total organic carbon (TOC) and CaCO3% had significant positive correlations with the total Se. A highly significant correlation was also found between the water-soluble Se and electric conductivity (EC), as well as with the water-soluble chloride, sulfate, nitrate, molybdenum, and sodium in soils. For the pedons tested, in general, both the total and water-soluble Se increased with depth. However, the water-soluble Se concentrations were greater in shallow than deep pedons where most Se was removed from soils with drainage water. It could be concluded that Se leaching from topsoils and that dissolving from Se-rich parent materials would be a major source of elevated Se concentrations in streams/rivers for the West-Central Colorado area. To minimize the impact on water quality, an appropriate land/water management practices should be followed to minimize Se leaching from soils derived from Mancos shale. 相似文献
15.
High soil selenium (Se) levels have been found in association with uranium deposits in Texas. A concern that high Se concentrations may be found in forages grown on reclaimed mine lands prompted this investigation. A native soil sampled near the mining area, and overburden materials sampled from two Se enriched uranium mine spoil sites were compared in a plant growth study in the greenhouse. Shoot yields and shoot Se concentration in each of ten grasses common to the region were determined from plants harvested three weeks after germination and from shoot regrowth harvested four weeks after the first harvest. Shoot weights were reduced for 5 of the 10 species growing in soils with medium and high Se status. Total shoot weights of Cynodon dactylon and Panicum coloratum from two harvests were consistently highest in all soil materials and are highly recommended for use as a stabilizing cover crop for lands disturbed from uranium mining. Generally, no correlation was observed between shoot weight and plant Se concentration or uptake in the 10 species. However, plant tissue Se concentrations in all species for at least one of the two harvest dates were above the 5 mg kg‐1 concentration considered potentially harmful to grazing livestock. Therefore, none of these species would be a suitable forage for livestock grazing on reclaimed Se‐enriched uranium mining overburden. 相似文献
16.
《Communications in Soil Science and Plant Analysis》2012,43(19-20):2669-2679
Abstract The adsorption of selenium (Se) in the selenate form and its desorption by phosphate in four soils with different physiochemical properties were studied in the laboratory. To determine adsorption isotherms for selenate 25 mL of solutions containing 1 to 100 ppm of Se were added to 2.5 g of soil. Desorption isotherms were determined by resuspending the samples in phosphate solution. The selenate sorption process was adequately described by the Freundlich equation. In pine forest and woodland soils, characterized by the highest organic matter content and cation exchange capacity (CEC) values, the isotherms were classified as L type, since the amount of Se sorbed appeared to move towards saturation. The organic matter content played the most important part in the adsorption of Se, while pH appeared to have a small effect on the ability of the soil to adsorb Se. The high CaCO3 content of the pine forest soil may have contributed in increasing the Se adsorption notwithstanding the high pH value. The cultivated and arable soils showed a reduced sorption capacity. The sorption could be described by an S type curve. At low concentrations of Se the affinity of the solid phase was less than that of the liquid phase. By increasing the concentration of Se in solution, the affinity of the solid phase increased and the sorption was favored. Selenate desorption by water was negligible, whereas the amount of Se desorbed by phosphate varied among the different soils. The desorption experiments indicated that a significant portion of the sorbed Se was irreversibly retained. This suggests the existence of linkages which allow the release of Se in the soil solution only after physico‐chemical variation such as exchange with phosphate ions. 相似文献
17.
青海东部农田土壤硒分布特征及其影响因素 总被引：2，自引：2，他引：0
植物中硒被认为是人体摄入硒的主要来源,而且大多数植物是从土壤中吸收硒。因此,不同地区土壤硒含量的高低直接影响到该地区食物中的硒含量。本研究以青海省平安地区农田土壤为研究对象,用原子荧光光谱法进行了土壤全硒含量和形态及价态的测定,对平安地区农田土壤全硒含量分布特征及其与成土母质、土壤类型的关系进行了研究。结果表明,平安地区土壤全硒含量变化范围为0.089~0.782 mg/kg,平均值为0.418 mg/kg,其中58%的土壤属于富硒土壤范畴。研究区域耕种淡栗钙土全硒含量最高,平均值为0.574 mg/kg;而灌淤黄土全硒含量最低,平均值为0.293 mg/kg。成土母质中,古近–新近系西宁群红色泥岩中硒含量最高,平均值为0.82 mg/kg。平安地区富硒土壤中硒的富集主要来源于古近–新近系西宁群红色泥岩风化。土壤中硒的赋存形态主要以有机结合态为主,铁锰氧化物结合态硒含量最少。可溶态硒和可交换态及碳酸盐结合态硒均以六价硒为主要赋存价态。平安地区富硒土壤中硒含量适宜,供硒潜力较大,且该地区受外界环境污染较少,具有良好的开发利用前景。 相似文献
18.
《Communications in Soil Science and Plant Analysis》2012,43(1-2):215-227
Abstract The experiment rationale was to determine forage micromineral concentrations as effected by biosolids fertilization. We determined the effects of two exceptional quality biosolids on bahiagrass trace mineral concentrations as related to beef cattle requirements. Twenty‐five 0.8‐ha pastures were divided into five blocks. Two biosolids were applied as normal and double agronomic rates. The control received NH4NO3. Forages were analyzed for total copper (Cu), iron (Fe), manganese (Mn), zinc (Zn), molybdenum (Mo), cobalt (Co), and selenium (Se), and soils were analyzed for Mehlich I extractable Cu, Mn, and Zn. Some significant increases (P<0.05) in forage Co, Cu, Fe, Zn, and Se were observed at various sampling times, but the increases were generally small and biologically insignificant. Although forage Mo samples from pastures with the Tampa biosolids applied were consistently higher than the control (P<0.05), at no time did they approach levels considered toxic. Similar results were seen in forage Mn concentrations, with treatment Baltimore‐2X elevating (P<0.05) Mn concentrations as well. Deficiencies of Co, Cu, Zn, and Se are common in this Florida region and slight elevations due to biosolids treatment could be beneficial. Biosolids applied at the highest rates improved soil Cu and Zn concentrations above control soils and soil Mn was increased over the control at both sampling times for Baltimore‐2X. In relation to beef cattle requirements, the majority of forages were deficient in Co, Cu, Se, and Zn. In summary, biosolids fertilization slightly improved the micromineral status of forage and soil, without creating toxicity. 相似文献
19.
三峡库区(重庆段)土壤硒分布特征及影响因素 总被引：7，自引：4，他引：3
重庆是我国缺硒(Se)的重点区域,多目标地球化学调查采用现代分析测试手段进行土壤Se元素的分布及富集的研究,对特色农业资源的开发利用具有重要意义。以每4 km2 1个表层和每16 km2 1个深层土壤数据对三峡库区重庆段土壤Se分布特征及其影响因素进行了分析探讨。结果表明:三峡库区(重庆段)表层土壤Se含量在0.006~5.79 mg/kg之间,平均值为0.16 mg/kg,以缺Se或潜在缺Se为主,其分布面积达到73.19%,足Se面积为25.77%,富Se或Se中毒区域仅为0.16%;深层土壤Se含量在0.03~0.62 mg/kg之间,平均值为0.12 mg/kg,缺Se面积占到67.36%,潜在缺Se面积也占到20.68%。不同类型间以黄壤表层土壤Se含量最高,其次是石灰土,且与水稻土和紫色土存在着显著性差异。不同土地利用方式间以林地与建筑用地表层土壤中Se含量相对较高,但各土地利用方式间不存在显著性差异。表层土壤Se含量相对于深层土壤表现出明显的富集特征,富集面积达到76.97%,但以弱富集区域为主,占到总面积的56.93%。土壤有机质、总氮含量与表层土壤Se含量存在较好相关性;与主要重金属以及S的相关性分析表明,其存在着较强的伴生关系,以Cd的伴生关系最为密切。表层土壤Se含量随着海拔和坡度的增加而增加,随着pH的增加而减少。此外,Fe、Al也是影响表层土壤Se含量的重要因素。 相似文献