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物探与化探  2023, Vol. 47 Issue (4): 1118-1126    DOI: 10.11720/wtyht.2023.1201
  生态地质调查 本期目录 | 过刊浏览 | 高级检索 |
西藏白朗县农田系统硒含量特征及影响因素
多吉卫色(), 次仁旺堆, 尼玛洛卓, 周鹏, 尼玛次仁
西藏自治区地质矿产勘查开发局 地热地质大队,西藏 拉萨 850032
Characteristics and influencing factors of Se content in the farmland system in Bailang County, Tibet, China
Duo-Ji-Wei-Se (), Ci-Ren-Wang-Dui , Ni-Ma-Luo-Zhuo , ZHOU Peng, Ni-Ma-Ci-Ren
Geothermal Geological Brigade, Tibet Bureau of Geology and Minerals Exploration, Lhasa 850032, China
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摘要 

富硒土地开发在全国各地区普遍开展并取得显著成果,然而西藏地区目前尚无报道有关富硒的土地或作物。本文以西藏白朗县重点耕地区为研究对象,讨论土壤、作物中的硒含量特征及影响因素,支撑服务西藏高原地区的富硒土地开发及利用。结果表明,研究区土壤Se含量范围为(0.05~0.76)×10-6,高于西藏土壤背景值0.15×10-6;研究区76.83%土地面积为足硒,根据碱性土壤Se标准阈值(w(Se)≥0.3×10-6)划定,Se含量高于0.3×10-6的土地面积45.43 km2。进一步研究显示,富硒土壤分布区域青稞籽粒中Se含量范围为(0.017~0.17) ×10-6,平均含量为0.063×10-6,油菜籽籽粒中Se含量范围为(0.043~0.14) ×10-6,平均含量为0.078×10-6。富硒土壤区域根系土结果表明,涅如组地层控制着土壤中Se的来源,土壤Se和有效Se含量与N、P、碱解氮、速效磷等具有显著的正相关,而与pH呈显著负相关,说明土壤中的大量养分元素及pH值对Se的行为具有重要影响作用。综上,白朗县富硒土壤分布区域土壤环境质量良好,农作物中硒的含量较高,具有较好的发展高原富硒农产品的潜力。

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多吉卫色
次仁旺堆
尼玛洛卓
周鹏
尼玛次仁
关键词 土壤Se含量青稞影响因素西藏    
Abstract

The development of Se-rich land has been carried out in many regions of China, achieving remarkable results. However, no Se-rich land or crop has been reported in Tibet. This study analyzed the characteristics and influencing factors of the Se content in the soils and crops of the key arable land areas in Bailang County, Tibet, aiming to lend support to the development and utilization of Se-rich land in the Qinghai-Tibet Plateau. The results are as follows: The soils in the study area have a Se content of (0.05~0.76)×10-6, which is higher than the background value of soils in Tibet (0.15 ×10-6); 76.83% of the land in the study area has sufficient Se, and land in the study area with a Se content of greater than 0.3 ×10-6 covers an area of 45.43 km2, as determined according to the standard threshold of Se content in alkaline soils (w(Se)≥0.3 ×10-6). Further investigation shows that highland barley seeds have a Se content of (0.017~0.17)×10-6 (average: 0.063 ×10-6) and rapeseeds have a Se content of (0.043~0.14)×10-6 (average: 0.078 ×10-6) in the distribution area of Se-rich soils. As indicated by the root soil results of the zones with Se-rich soils, the Nieru Group controls the source of Se in soils, and Se and effective Se content in the soils are significantly positively correlated with N, P, alkali-hydrolyzable nitrogen, and rapid available phosphorus but is significantly negatively correlated with pH. These results indicate that the behavior of Se is significantly affected by a large number of nutrient elements in the soils and pH. Overall, the distribution areas of Se-rich soils in Bailang County have high soil environmental quality, crops with a high Se content, and great potential for the development of Se-rich plateau characteristic agricultural products.

Key wordsSe content in soil    highland barley    influencing factor    Tibet
收稿日期: 2022-04-19      修回日期: 2022-12-13      出版日期: 2023-08-20
ZTFLH:  X142  
  X825  
基金资助:中国地质调查局地质调查项目(DD20160313-22);西藏自治区科技计划项目(XZ202001ZY0042N)
作者简介: 多吉卫色(1983-),男,工程师,主要从事土地质量地球化学调查工作。Email:549229277@qq.com
引用本文:   
多吉卫色, 次仁旺堆, 尼玛洛卓, 周鹏, 尼玛次仁. 西藏白朗县农田系统硒含量特征及影响因素[J]. 物探与化探, 2023, 47(4): 1118-1126.
Duo-Ji-Wei-Se , Ci-Ren-Wang-Dui , Ni-Ma-Luo-Zhuo , ZHOU Peng, Ni-Ma-Ci-Ren . Characteristics and influencing factors of Se content in the farmland system in Bailang County, Tibet, China. Geophysical and Geochemical Exploration, 2023, 47(4): 1118-1126.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2023.1201      或      https://www.wutanyuhuatan.com/CN/Y2023/V47/I4/1118
Fig.1  研究区工作范围及采样点位
指标 样品数 最小值/10-6 最大值/10-6 算术均值/10-6 中位数/10-6 算术标准差/10-6 变异系数
表层土壤Se 1853 0.05 0.76 0.24 0.24 0.08 0.32
根系土壤Se 30 0.23 0.69 0.35 0.33 0.08 0.24
西藏土壤Se[7] 205 0.04 0.37 0.15 0.14 0.48
中国表层土壤Se[12-13] 376743 0 49.60 0.26 0.21 0.22 0.80
Table 1  研究区表层土壤硒含量统计
Fig.2  研究区表层土壤富硒土壤分布
Fig.3  富硒土壤区域植物全株样品中硒含量分布特征
地层 算术均
值/10-6
中位
数/10-6
标准差/
10-6
最大
值/10-6
最小
值/10-6
变异
系数
昂仁组
(K1-2a)
0.20 0.22 0.03 0.22 0.14 0.17
甲不拉组
(K1j)
0.22 0.22 0.01 0.24 0.21 0.06
宗卓组
(K2z)
0.20 0.18 0.08 0.44 0.14 0.40
涅如组
(T3n)
0.32 0.32 0.07 0.50 0.17 0.20
朗杰学群
(T3l)
0.20 0.21 0.04 0.24 0.16 0.19
穷果群
(T1-2q)
0.20 0.21 0.03 0.24 0.16 0.15
Table 2  不同地质体分布区表层土壤中硒含量特征
Fig.4  根系土全Se和土壤有效Se与土壤pH、有机质指标的关系
指标 N P Se Zn K2O 有机质
Se 0.371* 0.431* 1 0.370* 0.397* 0.294
有效硒 0.462* 0.645** 0.822** -0.007 0.283 0.416*
指标 pH 碱解氮 F 有效硫 速效磷 有效硒
Se -0.542** 0.237 0.467** 0.729** 0.341 0.822**
有效硒 -0.428* 0.493** 0.167 0.684** 0.445* 1
Table 3  硒与其他指标的相关系数
指标 水溶态 离子交换态 碳酸盐结合态 腐殖酸结合态 铁锰结合态 强有机结合态 残渣态 全硒
水溶态 1
离子交换态 0.986** 1
碳酸盐结合态 0.856* 0.777 1
腐殖酸结合态 0.839* 0.783 0.719 1
铁锰结合态 0.594 0.651 0.289 0.618 1
强有机结合态 0.192 0.103 0.189 0.352 -0.394 1
残渣态 0.933** 0.949** 0.804 0.731 0.616 -0.056
全硒 0.941** 0.905* 0.801 0.927** 0.487 0.424 0.856* 1
Table 4  土壤全硒与各形态硒相关性分析系数
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