{"_buckets": {"deposit": "71b6db0f-5d34-4d5f-bf0e-47d259c8224b"}, "_deposit": {"id": "6828", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "6828"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00006828"}, "item_9_alternative_title_19": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u8a00\u8a9e\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "Comparison of solute concentrations in soil water sampled by different methods"}]}, "item_9_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1998-12", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "9", "bibliographicPageStart": "1", "bibliographicVolumeNumber": "17", "bibliographic_titles": [{"bibliographic_title": "\u540d\u53e4\u5c4b\u5927\u5b66\u68ee\u6797\u79d1\u5b66\u7814\u7a76"}]}]}, "item_9_description_4": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "\u82b1\u5d17\u5ca9\u5730\u57df\u306e\u30ab\u30e9\u30de\u30c4\u6797\u3092\u5bfe\u8c61\u3068\u3057\u3066\u3001\u6e1b\u5727\u6cd5\u3068\u9060\u5fc3\u6cd5\u3092\u7528\u3044\u3066\u571f\u58cc\u6c34\u3092\u63a1\u53d6\u3057\u3001\u305d\u306e\u6eb6\u5b58\u7121\u6a5f\u30a4\u30aa\u30f3\u6fc3\u5ea6\u306e\u6bd4\u8f03\u3092\u884c\u3063\u305f\u3002\u307e\u305f\u9060\u5fc3\u6cd5\u3067\u306f\u3001\u7570\u306a\u308b\u5727\u529b\u6c34\u982d\u6761\u4ef6\u4e0b\u306b\u304a\u3051\u308b\u571f\u58cc\u6c34\u3092\u63a1\u53d6\u3057\u3001\u305d\u306e\u6eb6\u5b58\u7121\u6a5f\u30a4\u30aa\u30f3\u6fc3\u5ea6\u306e\u6bd4\u8f03\u3082\u884c\u3063\u305f\u3002\u305d\u306e\u7d50\u679c\u3001Na^\uff0b\u3001Cl^\uff0d\u3001NO_3^\uff0d\u6fc3\u5ea6\u306b\u3064\u3044\u3066\u3001\u6e1b\u5727\u6cd5\u306b\u3088\u3063\u3066\u63a1\u53d6\u3055\u308c\u305f\u30b5\u30f3\u30d7\u30eb\u306e\u5024\u306b\u6bd4\u8f03\u3057\u3001\u9060\u5fc3\u6cd5\u306b\u3088\u308b\u305d\u308c\u304c\u9ad8\u3044\u50be\u5411\u304c\u307f\u3089\u308c\u305f\u3002\u3053\u306e\u3046\u3061NO_3^\uff0d\u6fc3\u5ea6\u306f\u3001\u571f\u58cc\u30b5\u30f3\u30d7\u30eb\u306e\u4fdd\u5b58\u671f\u9593\u306b\u571f\u58cc\u4e2d\u306e\u6709\u6a5f\u7269\u5206\u89e3\u306b\u4f34\u3063\u3066\u4e0a\u6607\u3057\u305f\u3068\u8003\u3048\u3089\u308c\u308b\u3002\u4e00\u65b9\u3001Cl^\uff0d\u306b\u307f\u3089\u308c\u305f\u6fc3\u5ea6\u306e\u9055\u3044\u306f\u3001\u63a1\u6c34\u6cd5\u306b\u3088\u3063\u3066\u7570\u306a\u308b\u571f\u58cc\u6c34\u306e\u5727\u529b\u6c34\u982d\u3092\u53cd\u6620\u3057\u3066\u3044\u308b\u3068\u5224\u65ad\u3055\u308c\u308b\u3002\u305d\u3053\u3067\u3001\u5727\u529b\u6c34\u982d\u306e\u7570\u306a\u308b3\u7a2e\u985e\u306e\u571f\u58cc\u6c34\u306b\u304a\u3051\u308bCl^\uff0d\u6fc3\u5ea6\u3092\u6bd4\u8f03\u3057\u305f\u3068\u3053\u308d\u3001\u5727\u529b\u6c34\u982d\u5024\u304c\uff0d1000\uff5e\uff0d800cmH2O\u306b\u304a\u3051\u308b\u571f\u58cc\u6c34\u4e2d\u306eCl^\uff0d\u6fc3\u5ea6\u306f\u3001\u5727\u529b\u6c34\u982d\uff0d1000cmH2O\u4ee5\u4e0b\u304a\u3088\u3073\uff0d800cmH2O\u4ee5\u4e0a\u306b\u304a\u3051\u308b\u571f\u58cc\u6c34\u4e2d\u306e\u305d\u308c\u306b\u6bd4\u3079\u3066\u3001\u9ad8\u3044\u5024\u3092\u793a\u3059\u50be\u5411\u304c\u8a8d\u3081\u3089\u308c\u305f\u3002\u3053\u306e\u3053\u3068\u304b\u3089\u3001\u5727\u529b\u6c34\u982d\uff0d1000~\uff0d800cmH2O\u306b\u304a\u3051\u308b\u571f\u58cc\u6c34\u304c\u3001\u84b8\u767a\u306b\u4f34\u3046\u6fc3\u7e2e\u306e\u5f71\u97ff\u3092\u6700\u3082\u53cd\u6620\u3057\u3066\u3044\u308b\u3053\u3068\u304c\u793a\u5506\u3055\u308c\u305f\u3002Soil water was sampled by suction and centrifugation to compare the solute ion concentrations of samples taken by these methods in Larix kaempferi forest underlain by granite in the Experimental Forest of Nagoya University, Aichi prefecture, central Japan. In the case of centrifugation, samples were taken under both high (\u03a8\u003e\uff0d1000 cmH2O) and low (\uff0d10000 cmH2O\u003c\u03a8\u003c\uff0d1000 cmH2O) pressure head conditions. Na^\uff0b, Cl^\uff0d, NO_3^\uff0d concentrations in the soil water sampled by the centrifugation were higher than those by suction. The difference in NO_3^\uff0d concentration between samples taken by the two methods is probably due to he decomposition of organic matter during the period from sampling to centrifuging. On the other hand, the difference in Cl^\uff0d concentration is probably caused by the difference in pressure head in the soil water sampled by these methods. The Cl^\uff0d concentration in the soil water under a pressure head from \uff0d1000 to \uff0d800 cmH2O is higher than that from 0 to \uff0d800\u3000cmH2O and from 0 to \uff0d800 cmH2O and from \uff0d10000 to \uff0d1000\u3000cmH2O. 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