38—1853.] 
THE AGRICULTURAL GAZETTE, 
op ecce now given y we are indebted to the kindani 
of Mr. H Pak — 
— — 
o Mr. LAN: whose re mark 
eeing 
A ds 2 ge of our deep 
arable Маб, se was to say 
case 
ceptional one), it was owing to the soil E - is 
d and ENTM. = the; nay wi 
capillar. 
а which it | 
ble as — as Dm e 
arks to Gra. 
render permea 
E perm Tn applying these rem 
t bear d there w 
s 
— had attained 
for sun and drought to 
harvest but 
ins, » was to 
mitted 
8 
у necessity for them * if water 
ely penetrated —. the surface into the rains, air 
: ment of Ire 
Q- 
to | for the беш of the wate 
fess have the sam 
that water found 
n 
vent the und 
the injur. 
|I contend, on the 
y o. ihr erops, I to 
2 
E E г pas Schal. with 
by the act of the surface water 
ac 
оса 
necessity for 
depths of drains in 
erned by the depth to which you 
late, be — in mind that if 
Water below your you 
ask where is you 
ater rising from ees 
d- 
‘ess and cause 
e;henee it arises that the 
— mils must be goy: 
unty, where 
taken off ‘by means of swa llow-holes | t 
r water rising M capillary attraction to , ail make their 
1 — — them. | bring 
way ultimately — al cma 
и them vegetable, animal, and 
cubie inch, ey — their share ; 
bave an envelope of 3 быр 0 
form a whitish slime 
combi make up the fertile and 
soils we find м the mouth of tidal rivers, as 
Thames, Hum 
Hi 
remar. 
0 uae " — үе 
of soils 
. 41 i dry or wet, heavy or 
stony, ae besides, The 
influences 
oet ofa used | to 0 be always considered. = 
as the drain drains will | 
draw effectively, and each cla ay. —— according to its re- 
quirements. Cheers.) In short, I do 
invalid land sufferi 
be 
erm 
arden e fact is, — 
a long drain, „` is — cud admit a 
a drain Lonce had 
ound no current ot air ; but Lighted a fire 
e drain and so current ; when 
il But if air is to 
be freely admitted at the ub of a drain, : te not 
tend all 
throughout ; I can alwa 
very often І cannot find it 
its way ом Ше by rising 
of w. water 
icularly, 
m a, wellon his 
which w — buried 10 feet in 
n soils A amu until 
4 small orifice being eaten e de. He could. not close 
Bis remapks manatee had 
he water bed tand 4 feet 
No 
pleasure he had 
пи of ете р building, and other 
ted by Mr. Denton. 
said—I have much satisfacti 
in being present — this тене to-day ; we have 
the advan antage of m on strong elay land before dis- 
cussing this important subject on the ppt I differ | o 
witt Dayis. an Denton that water 
enters from the m of Me drains, ug T. con меф т 
ind requir because the rain wai falls 
amp d the — 7 of the soil ; it falls below ren poin nt 
ce the soil sun and ai 
A8 to the bise of arte 
„1 сап say from, — —.— is y 4 т 
in! in this country. As 
id the ре of deep 
We 
e failure, it will be neces- 
instan to come = 
erwise 
time. SÉ will — 
* uniform deep draining in- 
зы. ЫР! the last 
‚ОЁ the, "Agricultural уча 8 у камык 
* ee a Denton 
e a ‘of T— ing | gro 
deeply, because you the 
ion, in 
еу are pleased to term it, — pre- 
on on the 
e supposi 
P 
f the land, and in strong retentive soils, wa 
uld not be had, u wax chanced to "hit on ris. 
He could sho ii Bie oU rsixp rsetshire, in 
the vale of Blackmoor, where they could get no water. 
off 
ays — water at 30 — when | t 
w.—Mr, Davis explained ing to 
ins 
accumu- 
d be the line | faet 
rom drain to drain, — if the drains were 4 feet a 
would from the su ineo 
- 
miler extreme and тет Л th chee 
Some 
ead. 
bein by a 
henaa it is more cesta: met it р 
Humie and 
ing 
be generally 1 That hat the organic is of 
les v vale to ——— 
e inorganic chere i is no doubt. 
organic c food in the soil, — this 4 
In Peru, Indian Morem grows where no organic 
exists in the soil ; again, Liebig has proved that plants 
ROYAL AGRICULTURAL. COLLEGE. 
CHEMISTRY, 
SESSIONAL ATION.—AGRI 
$WERS BY MB. Lo 
(2.). Tun rivers when. going nam rapid course 
atters organic . wit 
em, either in solution, as the former, or carried UM. 
by the current; on the mouths of rivers is deposited | i 
an vial soil is formed. 
gallons to hold in sclution two-thirds of a 
this is 0 | deposited on the banks of the Rhine ; H 
cy inermi of hieh are 
The ri too, by Le through so ws 
different strata ber M of 4 
me particles of each, an 
thus form a fertile soil. Besides, we find rain floods, &., 
experiments Денна ЧЇ» as Rear a 
one to —.— p they pe thot al al 
but not so tha 
The ce of organic food is the carbonic acid 
th чувел take, giving its oxygen baek, 
and retaining its gore which they no doubt assimilate 
; again, if we supply reb 
bonie aci acid, w * ind ih flourish - 
to sa 
the 
the inorganic — — be present, 
es before using. Again, am unceasing 
. oxygen for plants is the water, 
and they derive their nitrogen from the air; and 
