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Assessment of genetic classification and development suitability of natural selenium-rich soil |
LIU Dao-Rong1( ), JIAO Sen2 |
1. Zhejiang Geological Prospecting Institute,China Chemical Geology and Mine Bureau,Hangzhou 310002,China 2. China Chemical Geology and Mine Bureau, Beijing 100013,China |
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Abstract The formation of natural selenium-rich soiltends to be controlled by the parent materials. Spatially, it is closely related to the distribution areas of selenium-rich rocks such as black rock series, coal-bearing rock series, carbonaceous mudstones (shales), argillaceous limestones, and volcanic rocks. Selenium-rich soil of different genetic types greatly differs in development suitability. However,agenetic classification scheme of natural selenium-rich soil is yet to be developed. This paper sorted out the genesis of natural selenium-rich soil and divided it into three categories and 10 subclasses according to the major controlling factor of selenium source in soil (parent materials) based on existing classification schemes. Then it briefly reviewed the primary characteristics and development suitability of selenium-rich soils of four major subclasses, i.e., black rock series, coal-bearing rock series, volcanic rocks, and epimetamorphic rocks.Based on this, this study proposed assessment indices of the development suitability of natural selenium-rich soil.
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Received: 22 January 2021
Published: 15 December 2021
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类 | 亚类 | 主要成土母质类型 | 代表性地区 | 参考文献 | 沉积岩型 | 表生沉积型 | 全新世洪冲积物 | 浙江常山 | [14] | | | 湖沼相沉积物 | 浙江嘉善 | [15] | | | 湖相沉积物 | 浙江宁波 | [28] | | | 早中更新世红土风化物 | 浙江金华 | [26] | | 黑色岩系型 | 炭硅质岩类风化物 | 浙西地区,陕西紫阳,安徽石台, 湖北恩施,贵州开阳 | [13],[16],[29], [17],[19] | | 含煤岩系型 | 含煤岩系风化物 | 湖北恩施 | [17-18] | | 碳酸盐岩型 | 白云岩类风化物 | 滇中易门,贵州开阳 | [30],[19] | | | 泥质灰岩类风化物 | 浙北 | [10] | | | 灰岩类风化物 | 安徽 | [8] | | 碎屑岩型 | 泥页岩类风化物 | 赣南、青海东部 | [25],[31] | | | 砂泥岩类风化物 | 广西北部湾、江西丰城 | [27],[32] | | | 石灰性紫色泥岩类风化物 | 浙北 | [10] | 岩浆岩型 | 侵入岩型 | 酸性侵入岩类风化物 | 福建寿宁、海南 | [20-21] | | | 中性侵入岩类风化物 | 广东台山 | [33] | | | 基性—超基性侵入岩类风化物 | 广东台山 | [33] | | 火山岩型 | 酸性火山岩类风化物 | 福建寿宁、浙东沿海 | [20],[34] | | | 中酸性火山岩类风化物 | 福建寿宁、浙东沿海 | [20],[34] | | | 玄武岩类风化物 | 海南 | [21] | | 次火山岩型 | 酸性—中酸性次火山岩类风化物 基性—超基性次火山岩类风化物 | | | 变质岩型 | 浅变质岩型 | 千枚岩类风化物 | | | | | 蚀变凝灰岩类风化物 | 浙江常山 | [14] | | | 变质砂(泥)岩类风化物 | 海南 | [21] | | 中深变质岩型 | 板岩类风化物 | 滇中易门 | [30] | | | 片岩类风化物 | 海南 | [21] | | | 角闪岩类风化物 | 浙江龙游 | [35] | | | 黑云斜长片麻岩类风化物 | 浙江龙游 | [35] |
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Genetic classification of natural selenium-rich soils
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要素 | 评价标准 | 开发适宜性 | 赋值 | 富硒土地面积 | ≥300亩 <300亩 | 适宜 不适宜 | 3 0 | 地形地貌 | 平原、盆地等地势平坦,坡度<6° 谷地、丘陵、岗地等地势起伏较小,坡度6°~15° 山地等地势起伏大,坡度>15° | 适宜 较适宜 不适宜 | 3 1 0 | 集中连片程度 | 富硒土地集中连片,土地利用现状图斑细碎化程度低 富硒土地相对集中,图斑细碎化程度中 富硒土地分散,图斑细碎化程度高 | 适宜 较适宜 不适宜 | 3 1 0 | 农作物富硒率 | ≥70% <70% | 适宜 不适宜 | 3 0 | 农业生产设施条件 | 排涝能力强,基础设施完备,周边无潜在污染源 排涝能力中等,基础设施基本齐全,周边无潜在污染源 排涝能力低,基础设施不齐全,周边可能有潜在污染源 | 适宜 较适宜 不适宜 | 3 1 0 |
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Suitability evaluation of green selenium-rich land development factors
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