• TABLE OF CONTENTS
HIDE
 Copyright
 Contents






Group Title: Research report - Bradenton Agricultural Research & Education Center - GC1976-12
Title: Physiological effects of high soluble salts on plant growth
CITATION PAGE IMAGE ZOOMABLE PAGE TEXT
Full Citation
STANDARD VIEW MARC VIEW
Permanent Link: http://ufdc.ufl.edu/UF00067703/00001
 Material Information
Title: Physiological effects of high soluble salts on plant growth
Series Title: Bradenton AREC research report
Physical Description: 2 leaves : ; 28 cm.
Language: English
Creator: Woltz, S. S
Agricultural Research & Education Center (Bradenton, Fla.)
Publisher: Agricultural Research and Education Center, IFAS, University of Florida
Place of Publication: Bradenton Fla
Publication Date: 1976
 Subjects
Subject: Plants -- Effect of salt on -- Florida   ( lcsh )
Plants -- Soils -- Florida   ( lcsh )
Genre: government publication (state, provincial, terriorial, dependent)   ( marcgt )
non-fiction   ( marcgt )
 Notes
Statement of Responsibility: S.S. Woltz.
General Note: Caption title.
General Note: "October 1976."
Funding: Florida Historical Agriculture and Rural Life
 Record Information
Bibliographic ID: UF00067703
Volume ID: VID00001
Source Institution: Marston Science Library, George A. Smathers Libraries, University of Florida
Holding Location: Florida Agricultural Experiment Station, Florida Cooperative Extension Service, Florida Department of Agriculture and Consumer Services, and the Engineering and Industrial Experiment Station; Institute for Food and Agricultural Services (IFAS), University of Florida
Rights Management: All rights reserved, Board of Trustees of the University of Florida
Resource Identifier: oclc - 72469796

Table of Contents
    Copyright
        Copyright
    Contents
        Page 1
        Page 2
Full Text





HISTORIC NOTE


The publications in this collection do
not reflect current scientific knowledge
or recommendations. These texts
represent the historic publishing
record of the Institute for Food and
Agricultural Sciences and should be
used only to trace the historic work of
the Institute and its staff. Current IFAS
research may be found on the
Electronic Data Information Source
(EDIS)

site maintained by the Florida
Cooperative Extension Service.






Copyright 2005, Board of Trustees, University
of Florida




AGRICULTURAL RESEARCH AND EDUCATION CENTER
/ A, IFAS, University of Florida
Bradenton .
C Bradenton AREC Reseatch Report GCi976-12 October 1976

PHYSIOLOGICAL EFFECTS OF HIGH SOLUBLE SALTS ON lPLATrr GROWTH

SS. S. woltz


The two main effects of high soluble salt contents in the soil solution are:
First, to reduce or stop water uptake by roots, or even to cause a loss of water
from the roots to the soil; and second, to cause nutritional imbalances or toxi-
cities.

Osmotic pressure (OP), or water-pulling-power, is the key to the balance of
water movement between roots and soil solution. OP expressed in units of atmos-
pheres of pressure determines how readily water moves into roots or whether it
moves into roots or whether it moves out into the soil. The normal OP of plant
roots is in the range of 3-5 atmospheres. If the OP of the soil solution i less,
water is taken up; if more, it is lost. This is where the cotiept of "salt"' con-
centration becomes important. Thus, a plant with an average root OP of 4 atmos-
pheres would be in equilibrium with a salt solution of 5500 ppm and would take
up no water to replace any water loss from the top of the plant. If the OP in
the root zone were higher, the roots would lose water under any environmental
conditions.

Plants use more water, by far, than any of the other chemical compounds they
take up. They probably do not need to transpire large amounts of water for pur-
pose of growth and nutrition but plant leaves are "designed" for gas exchange,
especially of carbon dioxide and oxygen; water vapor is lost in the process but
does have a cooling effect on the leaf in the process of evaporating. They are
therefore quite vulnerable to excess water loss, with the resultant depletion of
available soil moisture.

The OP of most agricultural soils is less than 1 atmosphere except when they
are dry. The soil itself competes with the roots for water. As OP is increased
in nutrient solutions, water uptake by plants is decreased. There is an adapta-
tion, however, whereby plants from a lower OP solution are able to adjust when
moved to a higher OP solution by increasing their internal salt concentration.
Also, plants can adapt to a limited degree to increasing OP or salt content in
soil solution if the change is not too rapid.

Most species of plants do not develop normally when the soil solution OP
exceeds a few atmospheres (exceptions are xerophytes, desert plants and halophytes,
salt-tolerant plants). Mangrove trees, for example, can extract relatively pure
water from sea water by the expenditure of energy.

In addition to the effects on water uptake, salts from irrigation water may
produce nutritional imbalances and toxicities and may adversely affect the physi-
cal condition of soils. Sodium tends to make soils "run together,' to be wet,
non-aggregating and subject to poor drainage and aeration; light, sandy soils are
not affected greatly, however. Sodium also interferes with the uptake of other
positively charged ions that are nutritionally important including potassium,
magnesium and especially calcium. Excess sodium may induce calcium deficiency
or poor quality of plant products due to low calcium availability. Potential
toxic elements in irrigation water include boron, fluoride, lithium and bicarbonate.
In the case of boron, there is a need to learn how to fertilize properly according
to the amounts of boron present in the irrigation water. Analyses of water and
leaf samples will aid in clarifying this situation.
1









Large amounts of the negatively charged ion, bicarbonate, are desirable.
If bicarbonate is present much in excess df the chlride plus sulfate content, the
bicarbonate can cause the precipitation of calcium and magnesium and the production
of sodium-saturated soils that have poor physical condition. The bicarbonate ion
also increases the incidence of Ve deficiency.

In regard to the reduction or elimination of the effects of high soluble salts,
we may suggest the following procedures:

1. Avoid excess use of chloride, sodium and sulfate in fertilizer to reduce
the salt input of unnecessary elements.
2. Test your irrigation water and soils regularly to see if salt levels are
building up.
3. Select sources of water of the best quality available.
4. Provide good drainage to remove salts; leach as much as possible during the
rainy season,
5. Double row beds that are not thrown up too high are less subject to salt
damage for seeded crops. Salts move to the highest place in the bed or to the top
center of a double-row bed. Sloped beds may sometimes be used with seeding on the
downward side.
6. Be careful to avoid letting very light soils dry out since a 50% loss of
available soil moisture approximately doubles the salt concentration.
7. If a salt problem has been encountered especially in a heavier soil -
apply 1000 to 2000 lbs/A of gypsum to improve soil condition and help remove sodium
by subsequent leaching.
8. When possible, decrease the salt level in the soil by leaching even with
slightly salty water if necessary. With seep irrigation one may raise the water
level and then drain to help remove dissolved salts. Overhead irrigation is the
ideal way to remove salts by leaching. The saltier the water, the more leaching
one will have to do in order to use the salty water in production.
9. Salts accumulate in hard-pan subsoil pockets or depressions in the hard-pan
profile. These small areas that will damage a planting may be corrected by break-
ing the hard-pan at the center of the affected area and leaching out the salts or
by the use of tile drainage. The areas described will surprisingly persist even
with heavy rains or heavy irrigation in the absence of corrective measures.

A physiological character of root growth that has not been discussed is the
failure of roots to grow into a zone of high soluble salts because of water
limitations to the root. If fertilizer is placed too close to roots, they will
probably be burned, but roots will not grow into excessively salty soil, because
of the water deficit that occurs for these roots.

If soluble salts build up too high in soil, the plants will make little growth
and leaves may be burned. Plants grown under high salt conditions will have an
appearance as if they were grown in a drought with inadequate irrigation. They
will have dull-green leaves, slow rate of growth and poor yield of produce.




University of Florida Home Page
© 2004 - 2010 University of Florida George A. Smathers Libraries.
All rights reserved.

Acceptable Use, Copyright, and Disclaimer Statement
Last updated October 10, 2010 - - mvs