BOX 2.1. THE CRITICAL ZONE
The Critical Zone, depicted in Figure 2.1 , comprises the outermost
layers of the continental crust that are strongly affected by processes in the
atmosphere, hydrosphere, and biosphere. The upper boundary of the
Critical Zone includes the land surface and its canopy of lakes, rivers, and
vegetation, as well as its shorelines and shallow marine environments. On
land, the shallower part is the vadose zone, in which unconsolidated Earth
materials are intermixed with soil, air, and water. This porous medium is a
host for many chemical transformations mediated by radiant energy,
atmospheric deposition, and biological activity. Its storage capacity
influences runoff and groundwater recharge, affecting both the flow and the
quality of surface and subsurface waters. Within the vadose zone is the
pedosphere, a collective term for soils at the land surface. The
characteristic layering of the soil profile reflects the strong interaction of
climate and biota in the upper portion and the accumulation of weathering,
leaching, and decay products below. The water table marks the transition
from the vadose zone to the deeper groundwater zone, where the pore
space is filled by water. Like the vadose zone, the groundwater zone is a
chemically reactive reservoir. The lower limit of the Critical Zone generally
corresponds to the base of the groundwater zone, a diffuse boundary of
variable depth extending a kilometer or more below the surface. The volume
of water in the upper kilometer of the continental crust is an order of
magnitude larger than the combined volume of water in all rivers and lakes.
1 The Critical Zone is perhaps the most heterogeneous and complex region
of the Earth and the only region of the solid Earth readily accessible to
direct observation.
1 NRC, Opportunities in the Hydrological Sciences. National Academy Press,
Washington, D.C., 348 pp., 1991.
Global Climate Change and the Terrestrial Carbon Cycle
A significant amount of carbon is stored in soils and sedimentary rocks, thus
the Critical Zone plays a key role in the global atmospheric CO 2 balance. 1 Soil
constitutes the third largest carbon reservoir, and work with carbon-14 tracers
reveals that the distribution of soil organic matter strongly influences the means
and rate of carbon uptake and release. The exchange of carbon among
atmosphere, ocean, and terrestrial reservoirs is also affected by human land-use
practices and land-use histories (e.g., agriculture,
1 A U.S. Carbon Cycle Science Plan. A Report of the Carbon and Climate Working
Group, J.L. Sarmiento and S.C. Wofsy, co-chairs, U.S. Global Change Research Program,
Washington,
D.C.,
78
pp.,
1999
(
http://www.carboncyclescience.gov/
planning.html#plan ).
SCIENCE OPPORTUNITIES
38
About this PDF file: This new digital representation of the
original work has been recomposed from XML files created
from the original paper book, not from the original
typesetting files. Page breaks are true to the original; line lengths,
word breaks, heading styles, and other typesetting-specific
formatting, however, cannot be retained,
and some typographic errors may have been accidentally inserted.
Please use the print version of this publication as the authoritative
version for attribution.
The Critical Zone, depicted in Figure 2.1 , comprises the outermost
layers of the continental crust that are strongly affected by processes in the
atmosphere, hydrosphere, and biosphere. The upper boundary of the
Critical Zone includes the land surface and its canopy of lakes, rivers, and
vegetation, as well as its shorelines and shallow marine environments. On
land, the shallower part is the vadose zone, in which unconsolidated Earth
materials are intermixed with soil, air, and water. This porous medium is a
host for many chemical transformations mediated by radiant energy,
atmospheric deposition, and biological activity. Its storage capacity
influences runoff and groundwater recharge, affecting both the flow and the
quality of surface and subsurface waters. Within the vadose zone is the
pedosphere, a collective term for soils at the land surface. The
characteristic layering of the soil profile reflects the strong interaction of
climate and biota in the upper portion and the accumulation of weathering,
leaching, and decay products below. The water table marks the transition
from the vadose zone to the deeper groundwater zone, where the pore
space is filled by water. Like the vadose zone, the groundwater zone is a
chemically reactive reservoir. The lower limit of the Critical Zone generally
corresponds to the base of the groundwater zone, a diffuse boundary of
variable depth extending a kilometer or more below the surface. The volume
of water in the upper kilometer of the continental crust is an order of
magnitude larger than the combined volume of water in all rivers and lakes.
1 The Critical Zone is perhaps the most heterogeneous and complex region
of the Earth and the only region of the solid Earth readily accessible to
direct observation.
1 NRC, Opportunities in the Hydrological Sciences. National Academy Press,
Washington, D.C., 348 pp., 1991.
Global Climate Change and the Terrestrial Carbon Cycle
A significant amount of carbon is stored in soils and sedimentary rocks, thus
the Critical Zone plays a key role in the global atmospheric CO 2 balance. 1 Soil
constitutes the third largest carbon reservoir, and work with carbon-14 tracers
reveals that the distribution of soil organic matter strongly influences the means
and rate of carbon uptake and release. The exchange of carbon among
atmosphere, ocean, and terrestrial reservoirs is also affected by human land-use
practices and land-use histories (e.g., agriculture,
1 A U.S. Carbon Cycle Science Plan. A Report of the Carbon and Climate Working
Group, J.L. Sarmiento and S.C. Wofsy, co-chairs, U.S. Global Change Research Program,
Washington,
D.C.,
78
pp.,
1999
(
http://www.carboncyclescience.gov/
planning.html#plan ).
SCIENCE OPPORTUNITIES
38
About this PDF file: This new digital representation of the
original work has been recomposed from XML files created
from the original paper book, not from the original
typesetting files. Page breaks are true to the original; line lengths,
word breaks, heading styles, and other typesetting-specific
formatting, however, cannot be retained,
and some typographic errors may have been accidentally inserted.
Please use the print version of this publication as the authoritative
version for attribution.