基于时间序列的长江下游冲积平原区农田土壤质量演变特征

doi:10.16178/j.issn.0528-9017.20230493

浙江农业科学 ›› 2024, Vol. 65 ›› Issue (11): 2765-2771.DOI: 10.16178/j.issn.0528-9017.20230493

基于时间序列的长江下游冲积平原区农田土壤质量演变特征

韩林芮¹(), 胡丹阳¹, 宿宝巍¹, 张娅璐¹, 张欢², 高超¹^,^*()

1.南京大学地理与海洋科学学院,江苏南京 210023
2.南京师范大学海洋科学与工程学院,江苏南京 210023

收稿日期:2023-05-09 出版日期:2024-11-11 发布日期:2024-11-15
通讯作者: 高超(1962—),男,安徽六安人,教授,博士,研究方向为土地利用和水土环境效应,E-mail:chgao@nju.edu.cn。
作者简介:韩林芮(1998—),女,宁夏银川人,硕士,研究方向为土壤质量评价方法,E-mail:hanlinrui0309@163.com。
基金资助:
国家自然科学基金(41877002)

Evolution characteristics of farmland soil quality in alluvial plain area of lower Yangtze River based on time series

HAN Linrui¹(), HU Danyang¹, SU Baowei¹, ZHANG Yalu¹, ZHANG Huan², GAO Chao¹^,^*()

1. School of Geography and Ocean Science, Nanjing University, Nanjing 210023, Jiangsu
2. College of Ocean Science and Engineering, Nanjing Normal University, Nanjing 210023, Jiangsu

Received:2023-05-09 Online:2024-11-11 Published:2024-11-15

摘要/Abstract

摘要：

为揭示人类活动影响下土壤质量的演变趋势及其影响因素,在长江下游沿江平原典型区建立了0、60、160、280、2 000和3 000 a的土壤围垦时间序列,分析不同围垦时间与土地利用下土壤理化性质的差异。调查结果表明,围垦后表层土壤中的碳酸盐快速丧失,土壤逐渐由弱碱性转为弱酸性,围垦3 000 a后旱地土壤pH值约降低了2。长期水旱轮作的利用方式下,由于稻季土壤复盐基作用和氧化还原交替的状态,酸化程度略低。围垦之后相当长的一段时间内有机碳(SOC)、全氮(TN)和凯氏氮(AN)含量均呈逐渐积累的趋势,在表层土壤无机碳逐渐降低的同时,SOC含量比围垦前总体有所提高,表明耕作培肥措施在一定程度上有利于SOC和养分的积累。但围垦历史最久的圩区其SOC、TN和AN含量又有不同程度的降低,全磷(TP)和有效磷(AP)含量除在围垦初期有所升高,后期则不断降低。水旱轮作的利用方式下,土壤磷素的耗竭问题尤其突出,显示区内农田养分的投入处于不同程度的亏缺状态。目前的管理方式下,土壤肥力质量退化的现象应当引起足够的重视。

关键词: 冲积平原, 土地利用方式, 土壤质量演变, 土壤时间序列

Abstract:

In order to reveal the evolution trend and influencing factors of soil quality under the influence of human activities, soil chronosequence of 0, 60, 160, 280, 2 000 and 3 000 years were established in typical areas along the Yangtze River Plain in the lower reaches and the differences of soil physicochemical properties under different reclamation time and land use were analyzed. The survey results indicated that the carbonate in the surface soil was rapidly lost after reclamation, and the soil gradually changed from weakly alkaline to weakly acidic. After 3 000 years of reclamation, the pH value of the dryland soil decreases by about 2. Under the long-term rotation of water and drought, the degree of acidification is slightly lower due to the alternation of soil salinization and redox during the rice season. After a considerable period of time after reclamation, soil organic carbon (SOC), total nitrogen (TN), and available nitrogen (AN) contents showed a gradual accumulation trend. While the inorganic carbon in the surface soil gradually decreased, SOC overall increased compared with before reclamation, indicating that tillage and fertilization measures are beneficial to the accumulation of SOC and nutrients to a certain extent. However, the polder areas with the longest history of reclamation have varying degrees of decrease in SOC, TN, and AN contents. Total phosphorus(TP)and available phosphorus(AP)contents increase in the early stages of reclamation, but continue to decrease in the later stages. Under the use of water drought rotation, the problem of soil phosphorus depletion is particularly prominent, indicating that the input of nutrients in the farmland in the area is in a state of varying degrees of deficiency. Under the current management mode, the degradation of soil fertility quality should be paid enough attention.

Key words: alluvial plain, land use, soil quality evolution, soil chronosequence

中图分类号:

S153.4

韩林芮, 胡丹阳, 宿宝巍, 张娅璐, 张欢, 高超. 基于时间序列的长江下游冲积平原区农田土壤质量演变特征[J]. 浙江农业科学, 2024, 65(11): 2765-2771.

HAN Linrui, HU Danyang, SU Baowei, ZHANG Yalu, ZHANG Huan, GAO Chao. Evolution characteristics of farmland soil quality in alluvial plain area of lower Yangtze River based on time series[J]. Journal of Zhejiang Agricultural Sciences, 2024, 65(11): 2765-2771.

图/表 5

图1 研究区采样点分布此图基于中华人民共和国自然资源部标准地图服务系统的标准地图(审图号:GS(2019)3333号)绘制,底图边界无修改。

Fig.1 Distribution of sampling sites in the study area

图2 土壤pH和电导率变化趋势

Fig.2 Trends in soil pH and electrical conductivity

图3 土壤无机碳和有机碳含量变化趋势

Fig.3 Trends in soil inorganic carbon and organic carbon content

图4 土壤全氮和凯氏氮含量变化趋势

Fig.4 Trends in soil total nitrogen and available nitrogen content

图5 土壤全磷和有效磷含量变化趋势

Fig.5 Trends in soil total phosphorus and available phosphorus content

参考文献 26

[1]	杜慧, 关舒文, 王美艳, 等. 基于文献计量法的土壤退化研究现状及热点分析[J]. 中国水土保持, 2020(3): 33-36.
[2]	张桃林, 李忠佩, 王兴祥. 高度集约农业利用导致的土壤退化及其生态环境效应[J]. 土壤学报, 2006, 43(5): 843-850.
[3]	GUO L C, XIONG S F, CHEN Y L, et al. Total organic carbon content as an early warning indicator of soil degradation[J]. Science Bulletin, 2023, 68(2): 150-153.
[4]	FERREIRA C S S, SEIFOLLAHI-AGHMIUNI S, DESTOUNI G, et al. Soil degradation in the European Mediterranean region: processes, status and consequences[J]. The Science of the Total Environment, 2022, 805: 150106.
[5]	SCHLESINGER W H. Evidence from chronosequence studies for a low carbon-storage potential of soils[J]. Nature, 1990, 348: 232-234.
[6]	陈留美, 张甘霖. 土壤时间序列的构建及其在土壤发生研究中的意义[J]. 土壤学报, 2011, 48(2): 419-428.
[7]	CREWS T E, KITAYAMA K, FOWNES J H, et al. Changes in soil phosphorus fractions and ecosystem dynamics across a long chronosequence in Hawaii[J]. Ecology, 1995, 76(5): 1407-1424.
[8]	黄成敏, 龚子同. 海南岛北部玄武岩上土壤发生研究 Ⅲ.元素地球化学特征[J]. 土壤学报, 2002, 39(5): 643-652.
[9]	HUA H, SHI Y, WANG R H, et al. Phosphorus adsorption, availability, and potential loss characteristics in an ultisol-derived paddy soil chronosequence, using a stirred-flow chamber study[J]. Soil Science Society of America Journal, 2023, 87(3): 485-497.
[10]	ZHANG H, YIN A J, YANG X H, et al. Changes in surface soil organic/inorganic carbon concentrations and their driving forces in reclaimed coastal tidal flats[J]. Geoderma, 2019, 352: 150-159.
[11]	赖忠平, 欧先交. 光释光测年基本流程[J]. 地理科学进展, 2013, 32(5): 683-693.
[12]	PRESCOTT J R, HUTTON J T. Cosmic ray contributions to dose rates for luminescence and ESR dating: large depths and long-term time variations[J]. Radiation Measurements, 1994, 23(2/3): 497-500.
[13]	AITKEN M J. Thermoluminescence dating: past progress and future trends[J]. Nuclear Tracks and Radiation Measurements, 1982, 10(1/2): 3-6.
[14]	GUILLAUME GUÉRIN, MERCIER N, ADAMIEC G. Dose-rate conversion factors: update[J]. Ancient Tl, 2018, 29: 5-8.
[15]	鲁如坤. 土壤农业化学分析方法[M]. 北京: 中国农业科技出版社, 2000.
[16]	范德江, 杨作升, 毛登, 等. 长江与黄河沉积物中黏土矿物及地化成分的组成[J]. 海洋地质与第四纪地质, 2001, 21(4): 7-12.
[17]	李秀平, 方咸林. 无为县土壤有机质状况及提升途径[J]. 现代农业科技, 2013(7): 242-243.
[18]	张晨. 无为市2018—2019年度耕地质量现状及对策[J]. 安徽农学通报, 2021, 27(15): 134-136.
[19]	安徽省土壤普查办公室. 安徽土壤[M]. 北京: 科学出版社, 1996.
[20]	常新霞, 李文峰. 金沙江流域中上游土壤pH值空间分布特征[J]. 浙江农业科学, 2022, 63(8): 1900-1903.
[21]	刘畅, 周明华, 张博文, 等. 张家口坝上地区土地利用方式对土壤理化性质的影响[J]. 土壤与作物, 2021, 10(3): 333-343.
[22]	曹丽花, 郭祥坤, 连玉珍, 等. 信阳市不同土地利用方式下土壤团聚体及其有机碳分布[J]. 浙江农业科学, 2022, 63(4): 833-838.
[23]	KÖGEL-KNABNER I, AMELUNG W, CAO Z H, et al. Biogeochemistry of paddy soils[J]. Geoderma, 2010, 157(1/2): 1-14.
[24]	DING C F, DU S Y, MA Y B, et al. Changes in the pH of paddy soils after flooding and drainage: modeling and validation[J]. Geoderma, 2019, 337: 511-513.
[25]	ZHANG H, WU P B, YIN A J, et al. Organic carbon and total nitrogen dynamics of reclaimed soils following intensive agricultural use in Eastern China[J]. Agriculture, Ecosystems & Environment, 2016, 235: 193-203.
[26]	鲁如坤. 土壤磷素化学研究进展[J]. 土壤学进展, 1990, 18(6): 1-5, 19.

基于时间序列的长江下游冲积平原区农田土壤质量演变特征

Evolution characteristics of farmland soil quality in alluvial plain area of lower Yangtze River based on time series

RichHTML

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

图/表 5

参考文献 26

相关文章 5

编辑推荐

Metrics

本文评价

[1]	陈振华, 柳丹, 丁枫华, 朱阳春, 曲浩. 河套灌区不同尺度土壤氮含量的空间异质性分析[J]. 浙江农业科学, 2023, 64(10): 2549-2554.
[2]	曹丽花, 郭祥坤, 连玉珍, 房小玲. 信阳市不同土地利用方式下土壤团聚体及其有机碳分布[J]. 浙江农业科学, 2022, 63(4): 833-838.
[3]	谢元贵, 廖小锋, 肖玖军, 朱红苏, 董艳艳. 黔东南低中山丘陵地区典型小流域土壤理化性质研究[J]. 浙江农业科学, 2017, 58(8): 1477-1480.
[4]	原一荃，王繁*. 杭州湾南岸围垦区土壤有机碳空间分布特征及其影响因素[J]. 浙江农业科学, 2016, 1(2): 284-.
[5]	沈立铭1，张建锋2*，陈光才2，吴灏2. 不同土地利用方式对盐碱地土壤特性的影响[J]. 浙江农业科学, 2014, 1(8): 1246-.