Ecology and Environmental Sciences ›› 2025, Vol. 34 ›› Issue (10): 1569-1578.DOI: 10.16258/j.cnki.1674-5906.2025.10.007
• Research Article [Ecology] • Previous Articles Next Articles
CHEN Xinyi(), MAO Yaruo, SONG Liangying, WANG Tongyao, LI Qiquan*(
)
Received:
2025-03-06
Online:
2025-10-18
Published:
2025-09-26
通讯作者:
E-mail: 作者简介:
陈鑫怡(2001年生),女,硕士研究生,主要研究方向为土壤质量时空变化。E-mail: 2854626980@qq.com
基金资助:
CLC Number:
CHEN Xinyi, MAO Yaruo, SONG Liangying, WANG Tongyao, LI Qiquan. Characteristics of Spatial Distribution of Total Phosphorus in Cropland Soils and Its Main Controlling Factors in the Sichuan Basin[J]. Ecology and Environmental Sciences, 2025, 34(10): 1569-1578.
陈鑫怡, 毛雅若, 宋靓颖, 王童瑶, 李启权. 四川盆地耕地土壤全磷空间分布特征及其主控因素[J]. 生态环境学报, 2025, 34(10): 1569-1578.
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URL: https://www.jeesci.com/EN/10.16258/j.cnki.1674-5906.2025.10.007
分区方式 | 分区名 | 样点个数 | 最小值/(g·kg−1) | 最大值/(g·kg−1) | 平均值±标准差/(g·kg−1) | 变异系数/% | 偏度 | 峰度 | 数据分布类型 |
---|---|---|---|---|---|---|---|---|---|
全区 | 四川盆地 | 4409 | 0.30 | 3.92 | 1.59±0.51 | 32.27 | 0.46 | 0.66 | 正态分布 |
涪江流域 | 523 | 0.53 | 3.70 | 1.84±0.41a | 22.24 | 0.48 | 2.53 | 正态分布 | |
嘉陵江流域 | 496 | 0.67 | 2.97 | 1.49±0.35c | 23.22 | 0.52 | 1.07 | 正态分布 | |
流域 | 岷江流域 | 882 | 0.37 | 3.32 | 1.68±0.42b | 25.15 | 0.25 | 0.68 | 正态分布 |
渠江流域 | 836 | 0.42 | 2.47 | 1.25±0.31d | 25.22 | 0.22 | 0.08 | 正态分布 | |
沱江流域 | 881 | 0.39 | 3.82 | 1.82±0.50a | 27.72 | 0.33 | 1.00 | 正态分布 | |
长江干流区 | 791 | 0.30 | 3.92 | 1.48±0.66c | 44.74 | 0.63 | −0.07 | 正态分布 | |
成都平原区 | 491 | 0.78 | 3.82 | 2.16±0.45a | 20.86 | 0.58 | 1.20 | 正态分布 | |
地貌 | 川中丘陵区 | 2383 | 0.30 | 3.30 | 1.50±0.43c | 28.74 | 0.04 | 0.25 | 正态分布 |
盆周山区 | 1305 | 0.44 | 3.92 | 1.59±0.54b | 33.93 | 0.63 | 0.60 | 正态分布 | |
平行岭谷区 | 230 | 0.42 | 2.47 | 1.28±0.39d | 30.28 | 0.11 | −0.05 | 正态分布 |
Table 1 Statistical characteristics of total phosphorus content in surface soil of arable land in Sichuan Basin
分区方式 | 分区名 | 样点个数 | 最小值/(g·kg−1) | 最大值/(g·kg−1) | 平均值±标准差/(g·kg−1) | 变异系数/% | 偏度 | 峰度 | 数据分布类型 |
---|---|---|---|---|---|---|---|---|---|
全区 | 四川盆地 | 4409 | 0.30 | 3.92 | 1.59±0.51 | 32.27 | 0.46 | 0.66 | 正态分布 |
涪江流域 | 523 | 0.53 | 3.70 | 1.84±0.41a | 22.24 | 0.48 | 2.53 | 正态分布 | |
嘉陵江流域 | 496 | 0.67 | 2.97 | 1.49±0.35c | 23.22 | 0.52 | 1.07 | 正态分布 | |
流域 | 岷江流域 | 882 | 0.37 | 3.32 | 1.68±0.42b | 25.15 | 0.25 | 0.68 | 正态分布 |
渠江流域 | 836 | 0.42 | 2.47 | 1.25±0.31d | 25.22 | 0.22 | 0.08 | 正态分布 | |
沱江流域 | 881 | 0.39 | 3.82 | 1.82±0.50a | 27.72 | 0.33 | 1.00 | 正态分布 | |
长江干流区 | 791 | 0.30 | 3.92 | 1.48±0.66c | 44.74 | 0.63 | −0.07 | 正态分布 | |
成都平原区 | 491 | 0.78 | 3.82 | 2.16±0.45a | 20.86 | 0.58 | 1.20 | 正态分布 | |
地貌 | 川中丘陵区 | 2383 | 0.30 | 3.30 | 1.50±0.43c | 28.74 | 0.04 | 0.25 | 正态分布 |
盆周山区 | 1305 | 0.44 | 3.92 | 1.59±0.54b | 33.93 | 0.63 | 0.60 | 正态分布 | |
平行岭谷区 | 230 | 0.42 | 2.47 | 1.28±0.39d | 30.28 | 0.11 | −0.05 | 正态分布 |
模型 | 有效滞后 距离/km | 步长/ km | (块金值/基台值)/ % | 变程/ km | 决定系数 R2 | 残差 RSS | |
---|---|---|---|---|---|---|---|
球状 | 400 | 15 | 35.33 | 295 | 0.910 | 0.009715 |
Table 2 Semi-analysis of variance (ANOVA) of total phosphorus content in surface soil of arable land in Sichuan Basin
模型 | 有效滞后 距离/km | 步长/ km | (块金值/基台值)/ % | 变程/ km | 决定系数 R2 | 残差 RSS | |
---|---|---|---|---|---|---|---|
球状 | 400 | 15 | 35.33 | 295 | 0.910 | 0.009715 |
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