Explore: Soil Relationships
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AI-Generated Overview About “soil-relationships”:
Books Results
Source: The Open Library
The Open Library Search Results
Search results from The Open Library
1Shinrin no seikatsu
By Toshio Tsutsumi
“Shinrin no seikatsu” Metadata:
- Title: Shinrin no seikatsu
- Author: Toshio Tsutsumi
- Language: jpn
- Number of Pages: Median: 197
- Publisher: Chuo Koronsha
- Publish Date: 1989
“Shinrin no seikatsu” Subjects and Themes:
- Subjects: Forest soils - Plant - Soil relationships - Forest productivity
Edition Identifiers:
- The Open Library ID: OL12356794M
- Library of Congress Control Number (LCCN): 90156153
- All ISBNs: 9784121009432 - 4121009436
Access and General Info:
- First Year Published: 1989
- Is Full Text Available: No
- Is The Book Public: No
- Access Status: No_ebook
Online Access
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Wiki
Source: Wikipedia
Wikipedia Results
Search Results from Wikipedia
Soil
plants and soil organisms. Some scientific definitions distinguish dirt from soil by restricting the former term specifically to displaced soil. Soil consists
Plant and Soil
Plant and Soil is a monthly peer-reviewed scientific journal covering research on the relationships between plants and soil, such as relationships and interactions
From the Soil
quality" inherent in Chinese social relationships. In addition, he explains how kinship form the nexus of social relationships, governed under rules called guanxi
Structure–activity relationship
mathematical relationships between the chemical structure and the biological activity, known as quantitative structure–activity relationships (QSAR). A related
Soil fertility
Soil fertility refers to the ability of soil to sustain agricultural plant growth, i.e. to provide plant habitat and result in sustained and consistent
Soil zoology
inverse relationships between size and numbers of soil organisms. He also suggested that soil included water, air and solid phases and that soil may have
Soil pH
Soil pH is a measure of the acidity or basicity (alkalinity) of a soil. Soil pH is a key characteristic that can be used to make informative analysis both
Soil liquefaction
Soil liquefaction occurs when a cohesionless saturated or partially saturated soil substantially loses strength and stiffness in response to an applied
Soil salinity
Soil salinity is the salt content in the soil; the process of increasing the salt content is known as salinization (also called salination in American
Rhizosphere
region of soil or substrate that is directly influenced by root secretions and associated soil microorganisms known as the root microbiome. Soil pores in