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dtyland etap.
rath new notes that deep dtatnage plus gypsutn at
ttntate slowlyl sulphut wt“ testete aetdte soils, taut that
the leaehtng attt at salts that tallows may etteet sttsatn
health tntereeptor banks leadtng to “ER at nvet lseds
etteettvelv dean and pettntt teaching at the salted satls,
Where the pt-t ts more than ttst gypsutn tt alsa
tndieated ttt asststsodnttn tetnmal.
Whetever we tmgate wtth saline waters, we tnttst
tlush salt out at dratn the soils thatattghly, hut tn the
end she wanders tt etapptng an sueh settls ts tnevttahly
risky, and il dtverstpn lo enetgy ptaduettan vta nee
etaps, at the [mp and nyadeat antntal grazing ts not a
taettet use 0! dt-ylands tn pantculat, flood tmgatutn at
htrntwed nelds tan result tn a ma evipomflt'e watee
less, and a lwa» l0 seven-[um tnetease in salt mmznr
Iriholh Salt tn ttdge and tutraw systems of need
ttanawt ttrtgattan wtlt tnerease an the rtdges whete
less tlttshtng aeettts, Thus, tdeatty we should need the
ndges by cteattng heds wllh raised edges, and flush the
salt data to the tuttaws.
teeper tlmt nates the redueed ability 0! erapped
satls m tnitltt—tte tatnwatet, tn adtatntng ttelds. up ta 30
etn can he ahsettped by unenapped sells uvet a penad of
5 hours, while tn tdentteal empped Sell, only me an
ate ataserhed He notes that thesedtttetenets ate gteater
than these taetween dtttetent salt types wheatctapptng
ts thetetate at ttselt a tause ttt tneteased overland flows
and the subsequent neadtttg 0! lower so)! ptatttes, as ts
satl eatnpaet-ten by ovemrannx, and the use 0! hnvy
or last taran tnaehtnery
As [or pate spate, the speetltt gtavtty tsc.t at an
apen sott tt (mm ”He (equal to or gteatet than an
equal volume nt water) the s.c. ttt sull nttnetal
CmnpflnL-ms is 1 (r3 2 thus, the avetage atr pate spaee
tn the total valunta ts 50"» at ntnte (genuallv Matt,
tn a "dotted statl, all ttttt a tew at these pptes ate
walerrmledt lt that watet atsa eantatns salts, and de
flmuhliun aeeuts, the sntl enttntt sttueture qeteltly
ttteata dawn, and pates ate dogged wtth dtspetsed
stlty partteles, ln wheat lands, etttly me at the salt tnav
tse well—sttnetnted tttttnths at 0.75 ta 2 mm), whtle tn
treedratntng ttneleated stttls, me 0! the salt ls tatn-
pased at stteh parlichs
Thus. tt ts elear that the sttuttttte nt satlt under
dryland ettlttvattnn can in ttuth tateat down, and that
almost all the Soil pate spaee dtsappeats teven thaugh
enapptng tssttll passtttle at I27e entrnhstntehttel
A may)! taetar tn satl (mmb tannattan ts the ptesente
ol pnlysatehattdes Hottgrrham sugatst and gels
ptadueed by lttttnus, thts hutnte tnatenal ts etttteat |n
gaad wt] snuetute The wtdesptead ptaettee nthuttung
dtyland gtastes and wheat stuhtate tutther teduees the
stat htnntts Ftte ean aetttallv latte sttttaee salts sn that
they tattn tine dusts whteh blow at wash away. tttttnus
as green etap added ta neutral or alttaltne soils willt
huweter, testote ettttnb snuentre it salt watet defltknh
lattttn ean be stopped,
tn eattapsed sells, ttw and plant rnuts tape lwu tne
sepatattle ptatalents, even .t nat tlaaded. the reduced
pate spaees mnlain ltttle atr, tattt tn tatns, satl tarlxtn
dtaatde levels twaste gases hom mat respirattanl tnay
reaeh the level at 5% ttt is lvt tn tealthy satts. and-1. tn
air). This ts a lethal level tor plant mot growth As w¢|lt
Euphur—mncemmlmg (annembm hatterta ptetdttee
methane and sulphur dlnxlde ttnatsh gtasat as a ttsult
at tltedeeay ethntuus tn these anaentltte tdndtttats
Flnilly, the weakened plant tstdts are stttnett ta taptd
dtdttght film! by sttttate evapatattan, and taee estatmte
sness ttptn the salt water in the soil A patnt tarnea
where satl salts prevent water uptake by teats No
wander we ate tttttng nees and etaps thruttghmtt the
dwlands
lt ts MW atavtaus that to plant tnes m setts alteady tn
prtxess at eallapse ts hutle We need to stop the pm>
eess ttt soti enllapst tttelt, and H ts here that the
wash.” gmup have evolved what I helteve Io he a
ttntque and stteeesstttl West Auslnhan htll tattn
saltthan lo satl cellapse and desentneattan
Inmmr stats
tn earl r tnes. shallaw (0.5 tn deept comm»:
BANKS wete tnntt la stap salt tastes an stapes, Even
gentle slopes 0- at test lose soil tn tatn as tatntets n~
tnttve tree COVE! Beanie lower stapes get there water,
at flnwdown, satl etpstan ts nat ntueh less ml platns
than it ta on htll slopes at ltr or so Content hanks dtd
nut, hawetet. have a prntonttd etteet on WIN! etustun,
gully tannattan. ttee death. at sotl eallapse by tlapdrng
tndeed, salt L-vrnlually eauses eantaut bank: ta
eollapse, and nth-dtttlpadstwer thetn tn hzavy tatns
Although our salt pntttlents tnst appear in low (lat
ateas and valleys. the watet that eauses the ptnlsletn
easeades downslape The wt 5A LT appnaath is to
tttst taettle the ptalaletn at tts sonrce~|he htll tops
starting attaut tea tn helaw the ttdgeltnes and plateaus,
a deep t2 rat and wdde the; tnt dtteh ts lattlldoaed up
an eontottr Cate. tatten to that push all any tepsatl, ta
dtg tez tn down th s ttulldaaer lalade ta break up the
tansteted sttttsmt ttt ts otten neeedary to also rip), and
then m eetnpaet thls elayey and stany layer by
ramming it tirtnly against the dorm.“ taantt at the
dtteh, utteh and pant together are called an
INTERCEPIUR BANK trtgttte met.
It the dawnslape bank ts :Kedivdy sealed, all htgh
tuna" ox ttvetland flow stops at the dtteh. as does the
slnwer seepage at thraughttaw at the tepsatl, whteh
petehes on tap at the eantpaeted r horxznn as a
general seepage ltne. Na floodlllg at duwnslape sotl
results, and tutther satl eallapse eeases White the
htghet hank; ate tnade on the level as swales, dawn.
slape leanle slwpe at grades at 1-3000 ta natutal sheath
tteds, and thus bath salted and Itesh water are eats-ted
in sea tn sheaths withtn 24 veats, the stttps between
the hunts eatnntenee to regenerate grasses, and dytng
ttees tegatn health.
Ma ' etseptorttanlts, stttl an mmlmlrt ate “w bulll
every 3 at (vlflkll hetghtt downhlll ott stapes at
“345 at tnate, these term a eanttnuptts series at
ditches tptped at stdnettlled mt tnaehtnet-y (Whig
405