Changes in the soil pH, EC, available P, DOC and inorganic N after land use change from rice paddy in northeast Japan

P. N. Kusumawardani, W. Cheng, B. Purwanto, S. Utami
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引用次数: 5

Abstract

The objective of this study was to determine the changes in the basic soil chemical properties including pH, electrical conductivity (EC), available phosphorus (P), dissolved organic carbon (DOC) and inorganic Nitrogen (NH 4 + -N and NO 3 - -N) after approximately 15-40 years land use change from rice paddy field to orchard, wetland and upland in northeast Japan. Five land use change fields were investigated, including, forest, rice paddy, orchard, wetland and upland near Kumagai shrine, Shonai-machi, Yamagata, Japan. Soil samples were collected from surface layer (0-15 cm) and subsurface layer (15-30 cm) in October 2015. Soil chemical properties of pH, EC, available P, DOC and inorganic N (NH 4 + -N and NO 3 - -N) were analyzed on air-dried samples. The pH increased significantly in the upland after 15 years conversion from rice paddy in both layers, with other land use changes only increasing pH in subsurface layer. EC significantly decreased in the surface layer of orchard and upland fields and in subsurface layers of all the converted fields. Available P significantly decreased in the converted fields, except in the upland subsurface layer. DOC amounts were not significantly different after land use changes from paddy fields. The NH 4 + -N decreased significantly only in the surface layer of upland, while NO 3 - -N increased significantly only in the surface layer of wetland. Significant changes in soil properties were observed after 15 years conversion to upland and 40 years conversion to orchard and wetland from former rice paddy field in this study.
日本东北稻田土地利用变化后土壤pH、EC、有效磷、DOC和无机氮的变化
本研究旨在研究日本东北部稻田、果园、湿地和旱地土地利用变化后土壤pH、电导率(EC)、速效磷(P)、溶解有机碳(DOC)和无机氮(nh4 + - n和no3 - - n)等基本化学性质的变化。对日本山形县正内町熊谷神社附近的森林、稻田、果园、湿地和旱地5个土地利用变化场进行了调查。2015年10月采集表层(0 ~ 15 cm)和亚表层(15 ~ 30 cm)土壤样品。分析了风干土壤的pH、EC、速效磷、DOC和无机氮(nh4 + -N和no3 -N)的化学性质。15年旱地稻田化后,两层pH值均显著升高,其他土地利用变化仅使亚表层pH值升高。果园和旱地的表层和所有转化地的次表层的EC显著降低。除旱地次表层外,其余转化田有效磷含量均显著降低。不同土地利用方式下,稻田间DOC含量差异不显著。nh4 + - n仅在旱地表层显著降低,no3 - n仅在湿地表层显著升高。经过15年的旱地改造和40年的果园和湿地改造,土壤性质发生了显著变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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