草甸土
直接受地下水浸润并在草甸植被下发育的土壤。母质多为河流冲积物或地势起伏很小的洪积物或山坡坡麓地等。原始的草甸植被虽多已破坏，但草甸土式的发育仍在进行。草甸土的地下水位浅，层次分化明显。主要由完整的腐殖质层和有锈色斑纹的潴育层构成，有时下有潜育层。剖面中碳酸钙与盐分含量均不甚高。
41
Alias
Contributor
contributed at 2011-10-13
Classification(s)
●
Earth System(in Chinese) Soil Science
Detailed Description
| English |
|---|
| Name | meadow soil |
| Chinese |
|---|
| Name | 草甸土 |
| Description | 直接受地下水浸润并在草甸植被下发育的土壤。母质多为河流冲积物或地势起伏很小的洪积物或山坡坡麓地等。原始的草甸植被虽多已破坏，但草甸土式的发育仍在进行。草甸土的地下水位浅，层次分化明显。主要由完整的腐殖质层和有锈色斑纹的潴育层构成，有时下有潜育层。剖面中碳酸钙与盐分含量均不甚高。 |
How to Cite
NNU_Group (2011). 草甸土, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/42731ec4-6862-4ef8-a170-0ba3ff86e412
Copy
Copyright and Disclaimer
All copyrights of a material (model, data, article, etc.) in the OpenGMS fully belong to its author/developer/designer (or any other wording about the owner). The OpenGMS takes every care to avoid copyright infringement, contributor(s) should carefully employ materials from other sources and give proper citations.
