土壌の物理性
Online ISSN : 2435-2497
Print ISSN : 0387-6012
83 巻
選択された号の論文の7件中1~7を表示しています
  • ボードン パトリック, 漉澤 栄, 笹尾 彰, 酒井 憲司
    2000 年 83 巻 p. 3-16
    発行日: 2000年
    公開日: 2021/11/08
    ジャーナル フリー
    霞ヶ浦から浚渫される大量の底泥が,水田利用の大区画処理ヤードで天日乾燥固化処理されている。乾燥促進のための機械処理が求められており,底泥乾燥状態と地盤支持力を遠隔予測する必要がある。本研究は,表面情報により底泥乾燥状態を予測することを目的に実施した。浚深底泥の乾燥過程においては,乾燥の進行とともに土壌の凝縮が地表面からはじまり,更に3次元的な亀裂網の発生•発達及び大小さまざまな土塊が形成される。本報では,土壌水分変化に対する底泥亀裂と土塊の形態変化の関係を記述するため,亀裂網の幾何学的解析を行った。解析結果より,亀裂の形態特性値は水分減少とともに増大したが,土塊の形態特性値は土塊の数を除いて減少した。 8% d.b.の平衡含水比で亀裂の地表断面積が土塊の地表断面積の0.96倍になり,また亀裂/土塊の面積比と含水比との間には相関の高い指数関係が認められた。また底泥の亀裂パターンは乾燥速度と水分状態に依存することを認めた。
  • 駒村 正治, プアンペット ケットケオ, タナブド チャンチャイ, ヨンチャラチャイ チャオ
    2000 年 83 巻 p. 17-28
    発行日: 2000年
    公開日: 2021/11/08
    ジャーナル フリー
    We were defined a major change in land use and assessed consequent environmental impact in Songkhla lake basin, southern part of Thailand using remote sensing techniques for geographic information system applications. 35 percent of forest area in the basin was disappeared during 1982 to 1996, contributing to 22 and 76 percent increas in rubber and aquaculture areaes respectively. Consequently, the basin was deteriorated by soil erosion. It was estimated that the average rate of soil loss increased from 4.91 ha-1 y_, in 1982 to 7.21 ha-1 y_1 in 1996. The rate of soil loss was found higher in greater slope or rubber area. The destruction of forest cover disturbed hydrological function in the basin, caused soil erosion and increased sediment in Songkhla lake system.
  • 加藤 哲郎, 長谷川 功, 米田 和夫
    2000 年 83 巻 p. 29-40
    発行日: 2000年
    公開日: 2021/11/08
    ジャーナル フリー
    In the field of Kuroboku soil with humus top layer (Komekamito) at the Metropolitan Tokyo Agricultural Experiment Station (Tachikawa City) we investigated, in connection with the continuous application of organic matter, the effects of rotary tilling over a period of 20 years on the physico-chemical properties of surface soil and on crop yields. The results showed that the total carbon and total nitrogen contents of soil increased with the application of organic matter, but the rate of increase was smaller in tilling plot. In the plot where chemical fertilizers were continuously used, we found no effect of tilling on T-C and T-N. Available soil moisture content tended to decrease gradually over 20 years especially, the gaseous phase ratio at pF 1.5 tended to increase gradually, however, we observed a trend, as the years passed, that there were decreasing differences among the plots. Mineral nutrient content of the soil hardly differed between tilled and untilled soil, but it increased greatly in the plots where organic matter has been used repeatedly. Similarly to T-N of soil, available P2 05 increased with the continuous use of organic matter, but the rate of increase was lower in the tilled than in the untilled plot. Rotary tilling had little effect on the yields of cabbage and radish, though they were slightly higher with the continuous use of organic matter and the practice of rotary tilling. Even when chemical fertilizer alone was used, yields were higher when tilling was employed. Rotary tilling did not decrease crop yields. However, we noticed the formation of furrow pan due to rotary tilling, a tendency that was especially strong when only chemical fertilizers were used. Therefore 20 years of crop cultivation had no impact on the yields of cabbage and radish, but soil management that does not allow the formation of furrow pan is necessary, and for that reason the application of organic matter is important.
  • 長谷川 周一
    2000 年 83 巻 p. 41-46
    発行日: 2000年
    公開日: 2021/11/08
    ジャーナル フリー
    Field capacity is a widely used concept for irrigation management, but its definition is still controversial. Field capacity has been recognized by soil physicists a process of free drainage and it can not be defined as an intrinsic properties of the soil. To investigate further the meaning of field capacity, soil water content to a depth of 1 m and matrix flow by Darcy’s law at 1-m depth were measured and calculated every 30 minute for 1997 and 1998 at a maize-Chinese cabbage cropping field. Matric potential profiles with depth of a soybean field were also measured at a heavy rain event in 1991. The field soil is a well-drained volcanic ash soil. As the matrix flow is influenced by soil water content profiles during rain event and rainfall distribution pattern, the rain events whose amounts at the final day of consecutive rainy days were more than 10 mm/d, and brought the maximum values of matrix flow exceeding 5 mm/d at 1-m depth on the day following the rainfall were applied for discussing field capacity. When soil water conditions on the second day after the rainfall were applied as a field capacity, the matrix flow was 4 mm/d, and the hydraulic conductivity and the hydraulic gradient at 1-m depth were approximately 1X10-5 cm/s and 0.5, respectively. The amount of water stored to a depth of 1 m was 620 mm and the matric potential in the subsoil ranged between -50 to —100 cm. The matrix flow of 4 mm/d was very small compared to 620 mm water stored to a depth of 1 m. Although free drainage was still lasting on the second day after heavy rain events, the day can be applied as the field capacity for well-drained volcanic ash soils.
  • 中村 好男
    2000 年 83 巻 p. 47-57
    発行日: 2000年
    公開日: 2021/11/08
    ジャーナル フリー
  • 森 也寸志
    2000 年 83 巻 p. 59-65
    発行日: 2000年
    公開日: 2021/11/08
    ジャーナル フリー
  • 鈴木 創三
    2000 年 83 巻 p. 67-68
    発行日: 2000年
    公開日: 2021/11/08
    ジャーナル フリー
feedback
Top