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| Content Provider | Springer Nature Link |
|---|---|
| Author | Hashimoto, Shoji Suzuki, Masakazu |
| Copyright Year | 2004 |
| Abstract | Soil temperature is one of the most important factors governing biological activity in the soil. This study was conducted to investigate how forest clear-cutting changes soil temperature. Soil temperatures at 0.5, 1.0, 2.0, and 3.0 m depths were measured in two neighboring forest watersheds (35°12″N, 140°06″E) in Chiba Prefecture, Japan, from 1994 to 2000. One watershed was clear-cut 5 years after the observations began. After clear-cutting, the annual mean soil temperature at 0.5, 1.0, 2.0, and 3.0 m depths rose by about 2.2, 2.0, 1.7, and 1.4°C, respectively. The maximum respective soil temperatures rose by about 3.2, 3.0, 2.2, and 1.8°C. The minimum soil temperature rose slightly (≪1°C). The range of temperatures increased by 3.0, 2.4, 1.6, and 1.4°C, respectively. In our study, forest clear-cutting raised maximum and average soil temperatures but hardly changed minimum soil temperature. This is probably because solar radiation dominated in the summer season and increased soil temperature; on the other hand, net long-wave radiation, and releases of latent and sensible heat from the soil surface, were predominant in the cool season. |
| Starting Page | 125 |
| Ending Page | 132 |
| Page Count | 8 |
| File Format | |
| ISSN | 13416979 |
| Journal | Journal of Forest Research |
| Volume Number | 9 |
| Issue Number | 2 |
| e-ISSN | 16107403 |
| Language | English |
| Publisher | Springer-Verlag |
| Publisher Date | 2004-05-01 |
| Publisher Place | Tokyo |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Soil temperature Clear-cutting Microclimate Forestry Forestry Management Tree Biology Plant Sciences Plant Ecology |
| Content Type | Text |
| Resource Type | Article |
| Subject | Forestry |
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